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Dolomite clasts in clastic limestones
http://instruct.uwo.ca/earth-sci/fieldlog/GRANDFT/centrenature/stp1A_88.JPG
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-72.08706662247593,45.20455445247053,0 Ayers - road cuts 0 -72.06732820697174 45.2274231649893 0 3858.611139779133 1.352322186242993e-011 0.006134940042433963 #msn_ylw-pushpin_copy4002 -72.08281720464872,45.22624606528782,0 Ayers Cliff 1 - fuschsite 0 -72.07352769590122 45.18670167096215 0 1790.489563543377 0 0.1445396926447377 #msn_ylw-pushpin_copy1143 -72.07690583994784,45.18715538002914,0 Ayers Cliff 0 -72.03647837983588 45.16709105450628 0 5536.175926081703 3.637249965780493 0.009254943266215621 #msn_ylw-pushpin_copy0041 -72.03928366102886,45.16804638883199,0 Ayers Cliff quarry 0 -72.08265199640371 45.18450071749653 0 3745.074578779294 2.134300970800116e-010 1.110117429285129 #default_copy:0_copy58010020300 -72.08693770424691,45.18561734509898,0 Ayers Cliff - Ascot felsic volcanic rocks + fuchsite bear. debris flows 0 -72.06507678076292 45.18957516324566 0 3730.202438942861 0 0.1779158299111058 #msn_ylw-pushpin_copy440 -72.08482812030189,45.1857059478485,0 Bunker Hill 0 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Horizon schistose volcanics and sulphides 0 -71.89415094572992 45.36335614149012 0 2764.211475791416 0 0.5425551511785656 #khStyle71020100120 -71.89523953745879,45.3627019734289,0 Ascot mine 0 -71.90950802897184 45.32452926569609 0 2236.865337606012 0 0.531622219832364 #khStyle71020100120 -71.90992919798293,45.32468864474616,0 Sherbrooke - Chain Lakes 0 Rangeley 0 -70.64343939449165 44.96570179011181 0 330.128446200273 0 0.002275965267066964 relativeToGround #msn_ylw-pushpin_copy13006102 -70.64371409393327,44.96580329714183,0 Boil Mountain Stretched pillow lavas 0 -70.55823281907939 45.25696478032539 0 3844.450713503518 0.8389981108043403 -0.04802303966704634 #msn_ylw-pushpin_copy01200 -70.56015222061093,45.25755996191456,0 Boil Mountain cpxte 0 -70.58058761333797 45.27780592740358 0 701.2116550080832 78.80016656840678 -136.910187391935 #msn_ylw-pushpin011060 -70.57870461897051,45.27837176606806,0 Disraeli 0 -71.35624286995623 45.89960994019393 0 1340.709834543692 4.34720815196371e-011 0.9265436547647844 #khStyle702101011000 -71.35915881709268,45.89911624634517,0 schistose quartzites ?? 0 -71.43117029265326 45.91256645181614 0 5605.839092277094 2.026373849693936e-011 0.04167660001997033 #khStyle702101011000 -71.4282858118173,45.91798418379607,0 Dynamothermal aureole 0 -71.47545792045021 45.93201907136868 0 4588.420424768521 9.028631738619927e-013 0.009884999572106404 #khStyle702101011000 -71.48051056279513,45.92886034590863,0 Dynamothermal aureole section 0 -71.47902712044893 45.94699517010347 0 1687.6644765774 1.260764016799337e-011 0.007320846351874168 #khStyle702101011000 -71.47998924645381,45.94587643176262,0 Coleraine Breccia (conglomerate debris flow) 0 -71.37054742259105 45.96559128651536 0 5763.081303853854 6.17666794775585e-011 0.9143564997999679 #khStyle702101011000 -71.36849789870306,45.96605442815276,0 Lac de l'Est 0 -71.41717911689317 45.95195498505952 0 5578.29506346347 5.560803436100089e-011 0.8808285821069128 #khStyle702101011000 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3806.922598207207 68.89249187376045 -0.00676887662758324 #khStyle702101011000 -71.206695388748,46.01888546598379,0 Beauceville 0 -70.76907090772531 46.21933759160186 0 8430.039660076956 0.2113827984163798 0.5055763425935876 #khStyle702101011000 -70.77425331109008,46.21087861015617,0 Riviere des Plantes 0 -70.81339210493134 46.25713946830641 0 1442.956936732465 0.2113925656445513 0.4735726533380476 #khStyle702101011000 -70.8144025727462,46.25613621773771,0 Megantic 0 -70.88193988927445 45.57687788746171 0 4573.805398827147 21.807384442389 0.2404796898392235 #khStyle702101011000 -70.88475529137229,45.57765289833685,0 Woburn 0 -70.86068410896385 45.38568950492842 0 1930.910890323263 21.80738444235968 0.2555610615513257 #khStyle702101011000 -70.8596465187053,45.3835659141655,0 Notre-Dame-du-Bois Turn north off 212 0 -71.07050770462568 45.40112423678608 0 5122.663416411908 0 0.1062945165809644 #khStyle702101011000 -71.0729920198032,45.39455160497989,0 Clinton gabbros via Piopolis 0 -70.93615342432031 45.47093714852203 0 3503.19311931424 20.6793034548415 0.3243829095205124 #default_copy:0_copy62+nicon=http://maps.google.com/mapfiles/kml/pal3/icon63.png+hicon=http://maps.google.com/mapfiles/kml/pal3/icon55.png000300 -70.9484497909405,45.47129924173208,0 Clinton Mine?? 0 -70.91427096527082 45.42746350140195 0 5879.877541201206 0.4012433421089297 -0.008226803871407801 #default_copy:0_copy62000000 -70.92490719194237,45.42538747147233,0 Turn west off route du parc 0 -71.07329984161829 45.42378404524096 0 832.8014772855304 0 0.1043187871803475 #khStyle702101011000 -71.07226019399907,45.42381773235739,0 Chain Lakes 0 -70.69542787052414 45.35427094347543 0 3265.146950217887 21.80738444234933 0.3732526292011156 #khStyle702101011000 -70.69611407761738,45.35315355005803,0 Summit of Acadian intrusive body 0 -71.15233504050555 45.45615099137459 0 1019.087422522296 0 0.04802664863559139 #khStyle702101011000 -71.15233504050555,45.45615099137459,0 Border crossing 0 -70.80669912953114 45.3766124977123 0 1302.543754464605 21.80738444227142 0.294055426294579 #default211110100100110 -70.80749467053435,45.37818841890394,0 Maine 0 St John 0 -66.07469335735712 45.27469911432015 0 4205.802287743604 9.031679604313697e-012 1.156467433003671 #khStyle702101011000 -66.07740046831242,45.27532759536194,0 Calais 0 -67.32756760256223 45.16234713251136 0 41190.35939522363 0 2.030412627208089 #khStyle702101011000 -67.28376721804628,45.19025305328762,0 Bangor 0 -68.77047967012759 44.8046453149222 0 2797.802782402559 0.2114082127670529 1.901380010205645 #khStyle702101011000 -68.77061452886638,44.80236639706491,0 Penobscot 0 -68.71152212438824 44.46403825192351 0 335.5878580952809 0 0.03235982943768531 #khStyle702101011000 -68.71159169546621,44.464085592799,0 Castine 0 -68.79359631722674 44.39902607301978 0 9633.039732691756 4.655421193569565e-012 0.08400447200252224 #khStyle702101011000 -68.79614933671128,44.39204119007601,0 Bar Harbour 0 -68.20313706156654 44.38796900761582 0 880.0398638156679 2.059068611271856e-011 0.4961021847881152 #khStyle702101011000 -68.20313706156654,44.38796900761582,0 Cape Elizabeth 0 -70.23009490966797 43.60173416138214 0 15544.47187117574 3.906536243271396e-012 -4.940637916795209e-014 #khStyle702101011000 -70.19123877574839,43.55877873049083,0 Casco Bay 0 -70.35622663941268 43.49669566903628 0 15431.59743196609 5.523438204867522e-012 0.1168525152268137 #khStyle702101011000 -70.36146022314661,43.49583590953112,0 Portland 0 -70.2697323779384 43.66274379282622 0 4557.099339299477 1.233793492281987e-011 -0.009590620594859874 #khStyle702101011000 -70.27030739508142,43.66197551522259,0 Rangely 0 -70.6468023602785 44.96263854389897 0 3602.464199956754 0 -0.01315122017304311 #khStyle702101011000 -70.64470029757973,44.96647269732256,0 Stratton 0 -70.4492258389641 45.14281959267571 0 6225.766970010394 1.008399656536382e-011 0.3807077958463472 #khStyle702101011000 -70.44494467312188,45.14121835961628,0 Montreal - Noranda 0 Ste Anne, exit from 15 0 -74.10185175063116 45.88649497694727 0 2739.091755199726 0.001290604447521254 -0.2563250644437727 #khStyle5712191410001120 -74.10195716734492,45.88171919007503,0 St Sauveur, garnet anorthosite 0 -74.13741694524491 45.90399207909612 0 2715.384833860745 0.001290599720401311 -0.2818584525597374 #khStyle5712191410001120 -74.14106785679932,45.90435012710825,0 St Agathe layered opx anorthosite 0 -74.28693891102465 46.06233783533725 0 820.7166121328113 0 -0.393157241240816 #khStyle5712191410001120 -74.28921025120403,46.06360152219352,0 St Agathe lunch 0 -74.28693891102465 46.06233783533725 0 820.7166121328113 0 -0.393157241240816 #khStyle5712191410001120 -74.28662339804163,46.06019219830631,0 Mont Tremblant 0 -74.63942953912672 46.19216267787643 0 32117.74166398801 7.471648734525872e-012 -0.6472918017766911 #khStyle5712191410001120 -74.55359748195647,46.22449532784174,0 Mangerite 0 -74.67054598222742 46.12312640240506 0 1352.131729543622 0 -0.6699448249934367 #khStyle5712191410001120 -74.6729452718715,46.1226782254661,0 Labelle 0 -74.73179899263224 46.27983509754263 0 3413.772739863161 7.142999328436155e-012 -0.714543539301839 #khStyle5712191410001120 -74.72725192788417,46.27392313641976,0 Rd section with opx-peg, marble, restites 0 -74.80635914056043 46.36203289119511 0 8622.961216264312 0.5605491590855555 0.01062432960354429 #khStyle5712191410001120 -74.79093697695984,46.35436850400434,0 Basement gneiss, small quarry west side of road 0 -74.91075714478646 46.43750748319364 0 1022.759710077186 0 -4.233787509012859e-014 #khStyle5712191410001120 -74.90730384272146,46.437478497594,0 Lacoste 0 -74.91543238519249 46.43594005403607 0 11194.78141330319 0 -0.8472726906264201 #khStyle5712191410001120 -74.92550085106976,46.44808045802756,0 SteVeronique 0 -74.98878940895369 46.51543700660336 0 3433.335479318011 4.244448719643697e-012 -0.9004672014317984 #khStyle5712191410001120 -74.9861419014415,46.51502988847938,0 Tourmaline quartzites?? 0 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#khStyle5712191410001120 -76.15643239575307,46.79173847618131,0 Lac a La Veille 0 -76.24787247661041 46.80311578206502 0 19531.01170283216 3.47855025080948e-011 -1.815982709067914 #khStyle5712191410001120 -76.251864646801,46.79836023934256,0 Lac des Fourches Aphebian gneiss 0 -76.40103535582132 46.88824241750503 0 6505.362712442198 2.251254911784468e-011 -1.927730549092402 #khStyle5712191410001120 -76.39384891226169,46.88316041073063,0 Lac Rolande 0 -76.44170764154208 46.95088863844306 0 3025.000533726118 3.84323099732224e-011 -1.957341454833354 #khStyle5712191410001120 -76.44123035132839,46.95443238032335,0 Le Domaine 0 -76.52539013658637 47.09205312435228 0 8226.470624417088 2.766953358150415e-011 -2.018848260521923 #khStyle5712191410001120 -76.53813902387074,47.07703084236691,0 Dorval 0 -77.08205506786375 47.44912373994909 0 3007.78644283586 2.060781953127064e-012 -2.427302661441159 #khStyle5712191410001120 -77.08205506786375,47.44912373994909,0 Garnet gneiss 0 -77.21911275026409 47.62680291083715 0 3516.862500828203 0 -0.1532094258262459 #khStyle5712191410001120 -77.2282650994709,47.61691374730735,0 McLauren Lake???? 0 -77.34112582467061 47.88246688275984 0 9689.571980915574 0 -1.752386342731299 #khStyle5712191410001120 -77.35547295539944,47.86520666116274,0 Lac a La Puce???? 0 -77.35713824301308 47.88235689292176 0 9688.968587306317 0 -1.76425634508944 #khStyle5712191410001120 -77.34576956668145,47.88516131877429,0 Louvicourt 0 -77.38165885289315 48.07038062632874 0 3503.390657976438 0 -0.2732924070776742 #khStyle5712191410001120 -77.38237736383681,48.07265059288173,0 Val d'Or 0 -77.79352614118724 48.10281620621131 0 8762.594967744539 0.001290514458504288 -2.948646141086905 #khStyle5712191410001120 -77.78785755938672,48.10251663356691,0 Malartic 0 -78.14593732718063 48.14341723025383 0 16939.6337865485 3.262318016050526e-011 -3.20633788533659 #khStyle5712191410001120 -78.12659918873126,48.13627786978773,0 Riviere Heva 0 -78.20961857674283 48.24306734728622 0 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-78.9068046245862,48.21819073611784,0 Noranda 0 -79.02111128634782 48.24310196767343 0 5484.873553538407 1.683321731694705e-011 -3.87670338663072 #khStyle5712191410001120 -79.01525802433696,48.24220316385163,0 Grenada Cemetry?? 0 -79.04213944703122 48.18030025003168 0 9358.88735115786 4.26283197223305e-011 -3.87448577975872 #khStyle5712191410001120 -79.04374078328196,48.19118825000838,0 Pillow lavas 0 -78.97626141289673 48.21648601850161 0 3400.394422775715 0 -1.454926804950491 #khStyle5712191410001120 -78.9756046843288,48.21516606044408,0 Carlyle sequence 0 -78.96953457271225 48.2182981652813 0 3344.868275263711 1.456298475339728e-011 -1.449911048435361 #khStyle5712191410001120 -78.96843245994207,48.220417961096,0 Jnct 101 and rd to Amulet 0 -79.05276390072166 48.30731435960547 0 2396.539706992005 0 -3.027493426568779 #khStyle5712191410001120 -79.04654695453887,48.30893987420308,0 Horne Mine 0 -79.03901392536537 48.25663267047779 0 9382.097103289807 0 -3.017225726870167 #khStyle5712191410001120 -79.01662471899441,48.25403652134838,0 Amulet Mine(s) 0 -79.07841461946249 48.31518722180722 0 3666.581358170365 0 -1.531566673098588 #khStyle5712191410001120 -79.0760500620934,48.31219353084278,0 Noranda - Sudbury 0 Maps 0 Potter Mine 0 -80.23045219500185 48.59548689814438 0 10462.98813077166 0.1346658895551951 -2.870324591808267 #default_copy:0_copy63+nicon=http://maps.google.com/mapfiles/kml/pal3/icon63.png+hicon=http://maps.google.com/mapfiles/kml/pal3/icon55.png00100 -80.21299767261466,48.59738072178195,0 Munro Township Komatiite??? 0 -80.20252251384548 48.59674933107623 0 2571.581928924394 0.1346633683675482 -2.849396041482501 #khStyle5712191410001120 -80.19931869109594,48.60210733629637,0 Timmins 0 Dome 0 -81.94749841369203 48.77955844739964 0 25770.98062439027 6.391063450251131e-013 0.0267696053246705 #m_ylw-pushpin_copy8001200 -81.97665333452092,48.79827158463611,0 Montcalm 0 -82.08860486628937 48.66532064478951 0 25767.3694152734 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-81.235158997298,48.46000620455758,0 Kirkland Lake 0 Photos 0 624 Bend outcrop 0 -79.70376282531305 48.00250582208498 0 1901.777230715823 24.27761220103307 0.0122990627320831 #khStyle5712191410001120 -79.70482261490092,48.0025894613272,0 Kerr Adison 0 -79.5781040267634 48.13805826599771 0 1897.176062974712 1.259232709204942e-011 -2.328372443282067 #khStyle5712191410001120 -79.5781040267634,48.13805826599771,0 Larder Lake 0 -79.71171086466754 48.10045887807964 0 730.3326291145527 1.011386103600797e-011 0.2401333121809744 #khStyle5712191410001120 -79.71236573714398,48.10030657952105,0 Dobie 0 -79.82330283662699 48.13256383835839 0 4219.115503979608 3.485523777463401e-011 0.1571212425488754 #khStyle5712191410001120 -79.82049911757493,48.13285556517469,0 Misema River 0 -79.93528176632023 48.15969394987817 0 2959.096918381771 2.362693028963434e-011 -0.004220033158427741 #khStyle5712191410001120 -79.93269203044224,48.15497950008238,0 King Kirkland 0 -79.9573926894308 48.16253664366035 0 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]]> -80.00946641573609 48.15502024225463 0 8502.442690766469 2.027466318283196e-012 0.01137588259246632 relativeToGround #sn_icon63_copy561010 -80.02069258317107,48.15572139451052,0 Boston Creek Jnctn 6 and 112 south 0 -80.08394545740775 48.1211433145795 0 2894.471869937748 3.758084011240202e-011 -4.65852135257953 #sn_icon63_copy471200 -80.08596145789332,48.12033814661436,0 Boston Creek railtrack 0 -79.92912424006084 48.0165339784826 0 5750.028906768325 8.012732157107353e-025 0.3601041169770559 relativeToGround #msn_ylw-pushpin_copy091 -79.94267206265459,48.00940393299576,0 Turn off 112 to Boston Creek 0 -80.01678120437553 48.0099630057092 0 3288.866834412484 0 -4.608627690382768 #sn_icon63_copy51003 -80.01620893517082,48.00089222026869,0 Boston Creek auriferous quartz vein 0 -79.92922099317968 48.01648890152688 0 3263.9407601484 0 -4.543555210133222 relativeToGround #sn_icon63_copy420001 -79.92691619507957,48.01353116538716,0 Boston Creek beaver dam 0 Jim and the Beaver dam - http://instruct.uwo.ca/earth-sci/fieldlog/Kirkland_Lake/BostonC_Jim200.JPG -79.92922099317968 48.01648890152688 0 3263.9407601484 0 -4.543555210133222 relativeToGround #sn_icon63_copy600000 -79.92378240090454,48.01354641014052,0 Boston Creek Cpx.-komatiite 0 -79.92548770802013 48.01693063136521 0 5750.028906765496 0 0.3628068902373631 relativeToGround #msn_ylw-pushpin170120 -79.91545450341404,48.01674356257201,0 Swastika 0 -80.1303088534512 48.10125236052623 0 7216.619852399843 4.88312611013153e-011 -0.07140765083536485 #sn_icon63_copy55012 -80.10364378934332,48.10817360190436,0 Vigras Lake bas kom 0 -80.1303088534512 48.1012523605294 0 1239.977555488223 3.497550752264881e-011 -0.07140765083535254 #khStyle5712191410001120 -80.12769344221873,48.10093860558418,0 Timiskaming cong_sstns 0 -80.16950602298772 48.10201071860735 0 2276.627726536176 4.408238846903703e-011 -0.1005678936416698 #khStyle5712191410001120 -80.16781243667165,48.10415424532433,0 568 Railway station 0 -80.16950602298772 48.10201071860735 0 2276.627726536176 4.408238846903703e-011 -0.1005678936416698 #khStyle5712191410001120 -80.16720789768665,48.10761772589012,0 Jnct 101 with road south to Kirkland Lake 50 km+ 0 -79.81371456422167 48.52109646913783 0 3631.603818071578 2.532352073036891e-011 -4.457218313711616 #khStyle5712191410001120 -79.81873436334423,48.52088819714243,0 Englehart 0 -79.87438560640734 47.8204932224665 0 1125.232937467897 1.096637945997356e-011 -2.548395052165867 #khStyle5712191410001120 -79.87823799775048,47.82055188382491,0 Earlton 0 -79.81958052439759 47.71190010211052 0 3774.762765753529 2.259494210887932e-011 -2.507838905290929 #khStyle5712191410001120 -79.82444407543365,47.71069252518504,0 Haileybury 0 -79.63080697888258 47.43875837031243 0 2686.976406698542 0 -4.326702325598669 #khStyle5712191410001120 -79.62822858852645,47.44618043639959,0 Paleozoic Limestones 0 -79.69474632328327 47.51764981101187 0 2883.637389323465 0 -1.365391416163102e-011 relativeToGround #msn_ylw-pushpin_copy50002 -79.69727867674206,47.5109354001974,0 Timiskaming conglomerate 0 -79.66216957963758 47.4835409908798 0 3775.090834992018 9.609374711596916e-012 0.08322377227843839 relativeToGround #msn_ylw-pushpin_copy302301 -79.66998193025889,47.48303516638465,0 Large cross-beds in Timiskiming sandstones 0 -79.65480985648647 47.47840854163034 0 3777.511653021537 4.89757123412407e-012 0.08864712547630453 relativeToGround #msn_ylw-pushpin_copy06102 -79.66252781542002,47.47464212890332,0 Cobalt 0 Cobalt 0 Group photo - Norm, Jim, Michelle, Natalie, Alena<> http://instruct.uwo.ca/earth-sci/fieldlog/Huronian/Cobalt/cobalttrama195.JPG<>]]> -79.68604864659412 47.39217032155675 0 1981.068859032079 1.36461468520286e-011 0.4307432246836334 #sn_icon63_copy620001 -79.6897528392887,47.39265568940594,0 Stop 1 - differentiated top of a Nipissing diabase sill 0 -79.86579708642313 47.60278340022577 0 2645.29454758153 50.15110267671813 -0.1489194924938687 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy431030 -79.86898753717202,47.61035579503913,0 Stop 2 - typical Firstbrook Member 0 -79.72781796272103 47.44721881288016 0 2655.019294772988 45.58162830630985 0.03376503867392405 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy4802 -79.73015420818601,47.44530818661413,0 Silver veins, Cobalt 0 -79.68149858746786 47.391446260636 0 14707.74394774223 1.247626836338916e-011 0.06897983345417072 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy64000 -79.67974447809688,47.38408611955148,0 Maps 0 Cobalt region 0 94ffffff http://instruct.uwo.ca/earth-sci/fieldlog/Huronian/Cobalt/cobalt_Ows_f7.jpg 0.75 47.66935315170627 47.24956770362901 -79.48028883022005 -79.89050191601105 Cobalt area - general geology 0 91ffffff 1 http://instruct.uwo.ca/earth-sci/fieldlog/Huronian/Cobalt/Ows_f10.jpg 0.75 47.40188931340364 47.35151432151081 -79.63845069526431 -79.68866746579326 Stop 1 Nipissing Gabbro 0 http://instruct.uwo.ca/earth-sci/fieldlog/Huronian/Cobalt/Ows_f8.jpg 0.75 47.61224406886459 47.60856016023684 -79.86479935797338 -79.87056535243508 Stop 7 Cobalt 0 edffffff 3 http://instruct.uwo.ca/earth-sci/fieldlog/Huronian/Cobalt/Ows_f15.jpg 0.75 47.39114722031904 47.39064036547408 -79.68165856850987 -79.68256989136299 Stop 8 Cobalt geology east shore 0 STOP #8 SUMMARY TRAVERSE ACROSS TYPICAL COBALT AREA LITHOLOGIES This stop best illustrates the most common lithologies associated with the silver veins in the camp. The traverse is 90 over bedrock and serves to re-emphasize many of the features observed at earlier stops. Recent detailed mapping of the area, particularly with regard to sedimentological characteristics has been carried out by Rainbird (1980), Legun (1981) and Scammel and Mustard (1983). The mapping has resulted in a detailed fades division within the Coleman sequence. Subdivisions include two types of paraconglomerate, pebbly sandstone, laminated "varved?" siltstone and mudstone, non-cyclic siltstone, orthoconglomerate and basal breccia (Mustard, pers. comm., 1983). However, despite this segregation, a confusing mixture of these sediment-types remains at even smaller scales. Vertical contacts, laminite-draped depressions of short lateral extent, variable bedding attitude, recumbent folds and rapid changes in matrix composition and clast density (Legun, 1981) all.contribute to this problem. Coarsening-upward sequences, ripple marks, cross-bedding, sand dikes and other sedimentary structures are present and suggest a sub-aqueous out-wash or glacio-lacustrine delta environment of deposition (Legun, 1981). Basement rocks are variable in composition and include pillowed and massive mafic flows and intermediate to felsic volcanics. The unconformity is relatively non-descript. Huronian sediments are often "pasted" onto the basement rocks and are preserved as irregular, paper-thin outliers. Basal breccia occurs sporadically along the unconformity in thin narrow zones. The eroded base of a Nipissing diabase sill is inferred to have been within 50 m of the outcrop surface, A down-faulted remnant of the diabase is exposed immediately north of Cobalt. Points of Interest 8a: Contact between unaltered and altered pillowed mafic volcanics "Chlorite spotting" is sporadically developed within the volcanic rocks. The "spotting" is believed to form as a result of fluid migration associated with emplacement of the Nipissing diabase. In this particular instance, a fairly sharp, irregular contact demarcates the boundary between "spotted" and unspotted flows. The alteration is exceptionally intense here and illustrates a number of characteristics not commonly observed in spotted Huronian rocks. 8b: Chlorite alteration in mafic volcanic rocks Chlorite occurs in euhedral, rectangular shapes, in coalescing trains in fractures and stringers and as massive replacement within pillow selvages. The shape of the "spots" suggests that the chlorite has retrograded from previously formed, porphyroblastic growths of some mineral. Thin section analyses and microprobing provide few clues as to the original mineral composition. Spots are composed mostly of chlorite with accessory sphene, quartz, albite, biotite, fibrous amphibole, illmenite and pyrrhotite. Donaldson and Munro (1982) have suggested that the chlorite has grown as pseudmorphs after amphibole. A narrow, pre-Algoman, biotite lamprophyre dike has intruded the altered, pillow-volcanic flows. These dikes are common in the area and characteristically have very gentle dips. 8c: Basal breccia and orthoconglomerate The basal breccia is composed of angular fragments of the underlying basement lithologies. Fragments appear to have been tectonically brecciated. Fractured clasts have moved only slightly from original positions and can be pieced together. The matrix is composed of a mixture of the underlying Archean lithologies and the Coleman sediments. The top contact of the unit is often indistinct and gradational into the overlying rocks (Mustard, pers. comm., 1983). Fragments decrease in size upwards. The breccia is found only at the unconformity. It has short, lateral distribution and maximum thicknesses of 1.5 m (Rainbird, 1980). At this location, fragments from an underlying lamprophyre dike comprise part of the basal breccia. They trail to the north for a maximum distance of 2 m and indicate that minimal transport has taken place. Lindsey (1969) proposed that the breccia originated by glacial plucking or frost cracking. Donaldson and Munro (1982) suggest that the breccia represents a paleoregolith produced by mechanical weathering. Patterson (1979) described it as a paleosoil horizon and Rainbird (1980) suggested an origin due to slight gravity transport of frost heaved fragements and subsequent deposition as a talus-regolith in Archean depressions. Note the extensive development of chlorite alteration in the underlying pillowed volcanics and the distribution of the alteration within clasts and matrix of the overlying basal breccia and orthoconglomerate. Most "spotting" here is confined to fragments of the underlying rocks. Alteration may be controlled by varying pebble compositions and susceptibility to fluid migration or alteration may reflect processes active within the volcanic cycle rather than with the intrusion of Nipissing diabase. 8d: Cross-bedded sandstone Observe the cliff face to the east where good planar and trough cross-bedding is developed within medium to coarse-grained sandstone. Paleocurrent directions, as determined from these cross-beds, indicate transport in a southwest direction (Legun, 1981). 8e: Unconformity This exposure best illustrates the character of the unconformity between Huronian sediments and the underlying Archean basement. The basement is comprised of a variety of felsic volcanic rocks (possibly very silicified mafic volcanics), including bands of stretched siliceous and sericitic fragmental material. Skins of argillite and paraconglomerate occur as isolated patches. Numerous fractured wedges, with sharp, angular boundaries within the basement are infilled by these sediments. 8f: Cyclically laminated siltstone/mudstone These sediments are correlative with similar rocks exposed at stop #3. Thin parallel laminae «4cm) of green/grey siltstone and argillite display climbing ripples (Scammell, Mustard et al, pers. comm,. 1983), soft sediment deformation features and dropstones. The dropstones and varves are indicative of subaqueous, fresh-water deposition under floating ice (Legun, 1981). The return route illustrates many of the rapidly changing fades common to the Coleman Member unit. Problems encountered in mapping and interpretation of the original depositional environment are made apparent. 8g: Fragmental lamprophyre dike Post-Algoman intrusions of biotite lamprophyre are quite common. Contacts are often chilled and occasionally vesicular. In many instances, the wallrock has been ripped up and incorporated within the dike to form fragmental bodies. At this location, differential weathering of softer minerals creates a distinct pock-marked terrain. 2 http://instruct.uwo.ca/earth-sci/fieldlog/Huronian/Cobalt/Ows_f16.jpg 0.75 47.39712538050335 47.39143768204585 -79.67376121625611 -79.68025618032988 Temagami, Gowganda Fm unconformable on Archean sediments 0 -79.79542878212315 47.05833555888845 0 1733.767093626835 1.56684331180999e-011 -0.01629695193763476 relativeToGround #msn_ylw-pushpin_copy11032 -79.79645359247382,47.05661122383409,0 Jnct 11 and 64 from Field 0 -79.81118484033188 46.75038570817882 0 2283.144965331078 0 0.1509489479333683 #khStyle5712191410001120 -79.81163304389753,46.74942469861888,0 Field 0 -80.02565046747313 46.52072612198097 0 2484.593304329779 6.98407797368315e-012 -0.005057592811451902 #khStyle5712191410001120 -80.02659020889819,46.52173953877006,0 Sturgeon Falls jnct 17 and 64 north to Field 0 -79.94088170494159 46.36541595643536 0 3435.741787608855 0 0.05644009315097703 #khStyle5712191410001120 -79.93853879387316,46.3662343548068,0 North Bay 0 -79.42965581222863 46.33685558872971 0 45971.99475733599 2.006147578989739e-011 -4.172503222543842 #khStyle5712191410001120 -79.44423469612109,46.31852171198349,0 River_Valley 0
Davidson, A., Easton, R.M., Corriveau, L., and Martignole, J. 2002. Transect of the Southwestern Grenville Province. Field Trip Guidebook, May 30 – June 7 2002, Geological Association of Canada.

Easton, R.M., Davidson, A., and James, R.S. 2006. The Grenville Front tectonic zone and the River Valley area, Ontario. Friends of the Grenville Field Trip 2006.

Stop 7. Azen Creek Copper-Nickel-PGE Occurrence The Azen Creek zone was one of the initial discovery sites for PGE mineralization in the River Valley intrusion in the fall of 1998. Its location along the north contact of the intrusion, some 6 km from Dana Lake, was the first indication that PGE mineralization might occur discontinuously to continuously over a considerable strike length. The stripped area south of the road contains inclusions of medium-grained gabbronorite, troctolite, amphibolite, alkali feldspar granite and other felsic material within a medium-grained, grey-green olivine gabbronorite. Inclusions are more abundant on the west side of the stripped area, and vary from centimetre- to metre-scale. Mineralization consists of finely disseminated chalcopyrite and pyrrhotite in the matrix, as well as some sulphide-rich inclusions. Hrominchuk and Jobin-Bevans (2000) suggested that the inclusion-bearing zone might be intrusive into the contact zone of the intrusion, roughly coincident with the boundary between the fine-grained contact zone rocks and overlying divine-rich cumulates of the Olivine Gabbronorite zone (e.g.. Stop 5). The stripped area north of the road contains less mineralization, but shows a variety ofpegmatitic veins and pods. The pegmatitic pods are commonly cored by inclusions of felsic material, likely incorporated from the footwall of the intrusion. Return to vehicles, turn around, and retrace route to Highway 805.

0.0 km Junction with Highway 805, reset odometer to zero. Proceed west on Highway 805.

0.3 km Highway bends south, side road heads west to Upper Canada Stone Company and Giroux gravel pit. Note piles of crushed, black aggregate derived from the well-preserved gabbronorite of the River Valley intrusion. From this point westward, the road parallels the Sturgeon River on the south, as well as winding its way back and forth across an abandoned Canadian National Railways right-of-way.

1.4 to 1.1 km High ridges to the north of the road are well preserved gabbronorite of the River Valley intrusion.

5.4 km Outcrop ridge north of the road and the right-of-way consists of gabbronorite of the River Valley intrusion which contains 2 fabrics, the later fabric being parallel to the Sturgeon River. Rocks similar to these were previously mapped as being deformed equivalents of Nipissing gabbro (Dressier 1979), however, chemically and petrographically they belong to the River Valley intrusion.

6.8 km Road turns north at Glen Afton. Glen Afton lies near the eastern margin of the 1 to 2 km wide boundary zone that marks the Grenville-Southem Province boundary in this area. For the next 20 km. Highway 805 weaves back and forth across this boundary zone, exposing zones of intense mylonization separated by lenses of relatively well-preserved rocks of the Huronian Supergroup, the River Valley intrusion, and the Nipissing intrusive suite. Note that Highway 805 was re-aligned between 1988 and 1989; consequently, users ofDavidson's (1986) guidebook for'the Grenville Front in this area are cautioned that the distances and stop locations listed in that guide are not always easily determined. Where possible, this guide notes the location of some ofDavidson's stops.

7.0 km Park vehicles just past old railroad right-of-way and examine outcrops on west side of Highway.

Optional Stop. Huronian Metavolcanic Rocks

This is Stop 2.6 of Lumbers (1978). UTM for the south outcrop 554000E, 5166220N; for the north n outcrop 554005E 5166267N. The outcrop just north and west of the abandoned right-of-way consists of medium-layered dacite, which may be part of the Stobie Formation of the Huronian Supergroup. The low outcrop beside the road (100 m to the north) consists of felsic to intermediate pyroclastic rocks assigned to the Huronian Supergroup. These outcrops represent the easternmost extent of Huronian felsic metavolcanic rocks that have been recognized to date. It is difficult to differentiate fine-grained metavolcanic rocks from mylonitic rocks along the Grenville Front, due to the intensity of the deformation. Return to vehicles and continue north on Highway 805.

8.0-8.2 km Outcrops west of the highway consist of fine-grained amphibolite, possibly representing Huronian Supergroup metavolcanic rocks, whereas outcrops east of the highway, generally covered by vegetation, consist of deformed leucogabbronorite of the River Valley intrusion.

9.5 km Low outcrops of gneissic leucogabbronorite of the River Valley intrusion occur on both sides of the road.

9.8 km ATV trail to Lismer's Ridge area on property of Pacific North West Capital Corporation on the right (east). 10.1 to 10.6 km Outcrops in this stretch of road, particularly those on the north side of the road, represent an optional stop.

Optional Stop. Variably Preserved Nipissing Gabbro This location approximates Stop 2.7 of Lumbers (1978). The highway transects a body of Nipissing gabbro that has intruded the River Valley intrusion. Outcrop exposures on the north side of the road, in f /) the vicinity of UTM 554777E 516851 IN, exhibit varied degrees of preservation of the Nipissing rocks, similar to that observed in rocks of the River Valley intrusion. Dark green to almost black-weathering rocks are Nipissing gabbro retaining primary orthopyroxene and minor olivine grains, whereas green-weathering outcrops consist of typical, greenschist-grade, amphibolitized Nipissing gabbro, typical of what most of these rocks look like in the Southern Province. Note that plagioclase is much less abundant in the Nipissing rocks than in the River Valley intrusion. Return to vehicles and continue north on Highway 805.

10.7 km Outcrops north of road consist ofprotomylonitic gabbronorite of the River Valley intrusion and ultramylonite of unknown protolith.

10.9 to 11.1 km Outcrops east of the road consist of foliated to protomylonitic leucogabbronorite of the River Valley intrusion, intruded by deformed, pink felsite veins that are chemically similar to Huronian Supergroup felsic metavolcanic rocks (Easton 2003). UTM 554415E, 5168855N.

11.2 km Outcrop east of the road consists ofvaritextured gabbro of the River Valley intrusion. UTM 554500E.5169105N.

11.8 km Park vehicles and examine outcrops on east side of road.

Stop 8. Mylonitized Anorthosite of the River Valley Intrusion This is Stop R6a ofDavidson (1986) and Stop 2.8 of Lumbers (1978). Outcrops west of the road consist ofultramylonite derived from rocks of the River Valley intrusion. Please note a few large blocks in the area, in which mylonitic texture is developed in rocks that compositionally are anorthosite. Return to vehicles and continue north on Highway 805.

12.0-12.2 km Road extends uphill and around a curve, passing through outcrops of greenish weathering Nipissing gabbro. This curve is the location of stop R5 ofDavidson (1986).

12.3 km Outcrops on both sides of the road consist of black, flinty, ultramylonite of unknown protolith, but which may be derived, in part, from Huronian felsic metavolcanic rocks. This outcrop approximates stop R4 ofDavidson (1986).

12.5 km Outcrop west of road consists of boulder conglomerate, likely belonging to the Gowganda Formation, in contact with weathered granite of unknown age. Outcrops east of the road are a black, flinty ultramylonite (UTM 554057E, 5170254N). The section of road between kilometre 11.8 and 12.5 illustrates the rapid transition between weakly deformed and intensely deformed rocks within the Southern-Grenville province boundary. Metasedimentary and metavolcanic rocks of the Huronian Supergroup occur in close proximity to rocks of the River Valley intrusion in this area, but deformation has obscured primary contacts.

13.3 km Outcrops on curve consist of felsite and black, flinty ultramylonite.

15.1 km Pull over and park, examine outcrops on the east side of Highway 805.

Optional Stop. Mississagi Formation and Mylonitic Contact with the River Valley Intrusion This is Stop R3a and R3c ofDavidson (1986). Outcrops on the east side of Highway 805 consist of deformed quartz arenite of the Mississagi Formation. UTM of road outcrop is 554413E, 5172600N. / Proceed east through the bush for approximately 100 m to a cliff face. Black, flinty ultramylonite occurs at the base of the cliff, above quartz arenite of the Mississagi Formation. The mylonite is graditional upward, over about 1 to 3 m, into foliated leucogabbronorite of the River Valley intrusion. The Dana North zone, at the next field trip stop, occurs about 50 m stratigraphically above this location, and about 400 m east of this stop. Return to vehicles and continue north on Highway 805.

15.5 km Turnoff on right (east) leads to Pacific North West Capital Corporation Dana North exploration area.

16.3 km Junction, continue south roughly 500 m on road and park in flat area opposite large stripped . outcrop.

Stop 9. Dana Lake Copper-Nickel-PGE Occurrence

Prospectors L. Luhta, R. Bailey and R. Orchard first reported promising platinum-group element assay values from rocks of the River Valley intrusion near Dana Lake and Azen Creek in November 1998. Subsequently, Pacific North West Capital Corporation optioned and staked most of the north contact of the River Valley intrusion in Dana Township (inset map in Figure 12). Mustang Minerals Corporation optioned and staked most of the River Valley intrusion in Crerar Township, as well as part of the north contact near the Dana-McWilliams Township boundary. As of this writing. Pacific North West Capital Corporation has identified a dozen exploration targets along this northern contact. These are, from northwest to southeast, the Pardo, Dana North, Dana South, Banshee, Lismer's Ridge (Lismer's North and Lismer's South), Macdonald, Varley, Azen, Jackson's Flats, and Razor zones. The Thomson zone is located more centrally in the intrusion. Between 2000 and spring 2003, Pacific North West Capital Corporation, in conjunction with their partner, Anglo American Platinum Corporation Limited, had completed 5 diamond-drill programs. Approximately 288 diamond-drill holes totalling 58 000 m have been completed on their River Valley intrusion property in Dana Township. Diamond drilling was focussed almost entirely on the Dana North (see Figure 12) and Lismer's Ridge targets. A 6th diamond-drill program, aiming for a potential total of another 40 000 m of diamond-drill core, is underway, also focussing mainly on the Dana North and Lismer's Ridge zones (Pacific North West Capital Corporation, Press Release, April 10,2003; http://www.pfncapital.com/s/NewsReleases). The scope of these diamond drilling programs is too large to effectively summarize herein; consequently, the reader is referred to the comprehensive assessment file reports (Resident Geologist's office, Sudbury) related to these programs. Pacific North West Capital Corporation has released 2 Mineral Resource estimates for the Dana North zone, based on the Phase 1 to 5 drilling programs. In both cases, Derry, Michener, Booth and Wahl Consultants Limited conducted the resource studies. The first in situ resource estimate (Pacific North West Capital Corporation, Press Release, October 16, 2001) was a total measured, identified and inferred resource of 593 000 ounces palladium, platinum and gold at Dana North, Dana South and Lismer's Ridge. This estimate used a 0.7 g/t Pt+Pd cut-off grade, and can also be expressed as 12.7 million tonnes at 1.46 g/t Pt+Pd+Au. This can be broken down into 7.74 million tonnes at 1.60 g/t Pt+Pd+Au at Dana North and South, and 4.97 million tonnes at 1.24 g/t Pt+Pd+Au at Lismer's Ridge. The second Mineral Resource estimate (Pacific North West Capital Corporation, Press Release, October 17,2002) was a total measured and indicated resource of 825 900 ounces palladium, platinum and gold. There were inferred resources of 200 600 ounces palladium, platinum and gold, yielding a total of 1 026 500 ounces at Dana North and Lismer's Ridge. This estimate used a 0.7 g/t Pt+Pd cut-off grade, and can also be expressed as 18.1 million tonnes of measured and indicated at 1.36 g/t Pt+Pd and 5.4 million tonnes inferred at 1.11 g/t Pt+Pd. Roughly 60 of this resource is in the Dana North area. A description of the Dana North zone has been published by S. Jobin-Bevans, Projects Manager for Pacific North West Capital Corporation, in James et al. (2002b). The description below, in a slightly smaller font, is derived from that published report. The distribution of the marginal Inclusion-bearing/Breccia zone (roughly equivalent to the Inclusion- and/or Fragment-bearing zone ofHrominchuk (2000) and James et al. (2002a)), the loci of mineralization, is in abmpt, intrusive contact to the east with the Neoarchean-age Pardo gneiss, and to the west these zones are replaced by a weakly layered to massive leucogabbro-gabbro-melagabbro sequence. Small pod-like, alkalic intrusions of unknown age are observed at two places along the intrusive contact where they displace the Inclusion-bearing/Breccia Zone. As well, faults related to the Grenville Front and a 1238 Ma Sudbury swarm oli vine-magnetite gabbro dyke cut or displace this zone. Silicate assemblages that host the mineralization in this part of the River Valley intrusion exhibit upper greenschist facies mineralogy in contrast to the upper amphibolite facies and preserved magmatic assemblages that dominate the remainder of the intrusion. The stratigraphy of the Inclusion-bearing/Breccia Zone is normally -100 m wide in plan view. From the footwall Pardo gneiss, westward into the intrusion, the sequence and character of the distinguishable units are:
1 Footwall Breccia Unit: typically 5 to 15 m wide, but may be absent. It consists of partly rounded to angular, centimetre- to decimetre-size fragments of country rock (-75; Pardo gneiss, Archean gabbro, diabase, diorite minor Huronian Supergroup metasedimentary rocks) and River Valley intrusion material (-25; chilled gabbro and medium-grained melagabbro) in a matrix of finer grained rock of similar composition and (or) an aplitic to granitic matrix. A narrow zone ofmigmatite at the contact of the intrusion is probably due to contact metamorphism, and granitic veins can be traced from this unit into the footwall at Lismer's Ridge. Sulphide minerals are dominantly pyrite and pyrrhotite with local areas of trace to 1 volume percent chalcopyrite + pyrrhotite. Platinum group element concentrations are normally less than 25 ppb.
2 Boundary Unit: 5 to 20 m wide, but may be absent. It contains partly rounded to subangular, centimetre- and decimetre-size fragments of country rock (typically 10-25), and cognate xenoliths of melagabbro, gabbro and less commonly leucogabbro to anorthosite in a matrix of gabbro to melagabbro ± aplite/granite, as in the Footwall Breccia. Sulphide minerals are mainly pyrite and pyrrhotite, locally up to 3 volume percent chalcopyrite + pyrrhotite occur; platinum group element contents are typically <75 ppb with local concentrations greater than 1000 ppb.
3 Breccia Unit: 20 m wide to greater than 100 m. It contains as much as 95 dominantly cognate xenoliths of gabbro to melagabbro and subordinate leucogabbro in a medium-grained matrix of similar composition; fragments are partly rounded to round probably due to partial assimilation, and centimetre to decimetre in size Those greater than a metre are mainly footwall compositions (including Huronian Supergroup metasedimentary rocks) and tend to be larger with increasing proximity to the intrusive contact. Sulphide minerals (1 to 5 volume percent pyrrhotite + chalcopyrite) occur as both bleb and disseminated types; platinum group element contents are highly varied, but most values range from 500-6000 ppb with local concentrations greater than 10,000 ppb.
4 Inclusion-bearing Unit: 10 to 50 m wide. It contains >90 autoliths of leucogabbro, subordinate gabbro and less melagabbro in a matrix of either medium-grained leucogabbro or gabbro; the leucogabbro xenoliths are subangular to partly rounded, dominantly decimetre to metre in scale, and appear to be sloped inclusions from the adjacent (overlying) Leucogabbronorite zone. Sulphide minerals include trace to 3 volume percent pyrrhotite + chalcopyrite; platinum group element contents range from 100-500 ppb with local concentrations greater than 1000 ppb.
Interestingly, the Breccia Unit, which shows the highest and most persistent sulphide-associated platinum group element mineralization, has the smallest proportion of footwall inclusions (<1%); perhaps an indication that chemical contamination from footwall lithologies is not a major controlling factor on mineralization. Fine-grained gabbro and diabase dikes cut all of the above units as well as the Leucogabbronorite zone in the main part of the intrusion. These dikes are metamorphosed at a grade similar to the intrusion in the Dana North area and are distinct from younger dikes of the Sudbury swarm'.
Drill hole, data suggest that the dip of the contact of the Inclusion-bearing/Breccia zone with the footwall is at least 45° to 65° and toward the intrusion, whereas the apparent dip of the surface between the Inclusion-bearing Unit 7 and Breccia Unit is steeper (-70° ) and toward the intrusive contact. The attitude of metre-scale layering in the Leucogabbronorite zone adjacent to the mineralized Inclusion-bearing/Breccia zone is poorly constrained but is estimated to be near-vertical (-70° to 90° west and east) and possibly shallowing (i.e. less than 70° west dip) westward into the intrusion.
S/Se ratios for 13 of 15 samples (mineralized and barren) from the Dana North and Lismer's Ridge areas have values from 500 to 2120, which are well within the magmatic range indicted by the Merensky and J-M reefs, awl Konttijarvi-Portimo contact-type mineralization (i.e., 700-800 S/Se). Footwall rocks have low Pt, Pd and Au and Pd/Pt and Cu/Ni are less than 1; these metal values indicate that the Archean footwall rocks are not genetically related to the platinum group element mineralizing event(s). Estimates of the metal values for barren magma that forms large parts of the intrusion or which are feeders, have less than 100 ppm Cu and anomalous Pt + Pd concentrations averaging 32 to 35 ppb, but their metal ratios, Pd/Pt and Cu/Ni, are both less than 1, which is unlike mineralized samples (see below). Analytical data for sulphide-bearing felsic and mafic dikes and the Boundary, Breccia and Inclusion-bearing Units all show moderate to high average Pt+Pd (peaking in the Breccia Unit, as expected), and all show Pd/Pt and Cu/Ni ratios based on metal averages in the range 1.1-4.8, distinct from the low sulphide, Cu-poor assemblages. The mineralized zones at the Bull Frog Zone of the East Bull Lake Intrusion show the same geochemical features.

RVI PGE Metallogeny

Similar to the East Bull and Agnew lopoliths, the RVI is host to contact- and reef-type Ni-Cu-PGE mineralization. It occurs at the east end of what might be termed the Greater Sudbury Nickel Belt. A unique feature of this "metallotect" is that the associated Ni-Cu-PGE mineralization recurs in mafic igneous complexes over a considerable span of time: from early East Bull @ 2490-2475 Ma, through Nippissing @ 2215 Ma, to the Sudbury Event @ 1850 Ma. Outside of the Bushveld Complex in South Africa, this is undoubtedly the greatest known Ni-Cu-PGE anomaly on the globe and the cause for such Ni-Cu-PGE concentration is still open to considerable speculation. One might hypothesize that the East Bull magmatism was the most formative, with the Nippissing and Sudbury ores being derivative and inherited. It seems clear in the case of the East Bull Lake Suite, that the source magma attained sulphur saturation at an early stage in the filling history of the EBL chambers to account for repeated occurrence of contact-type ores. An interesting result of past and ongoing work on the EBL contact-type ores is the implication of early high temperature (1200° C) anorthositic plagioclase fractionation in developing a dense high Fe-Mg residual melt. Mixing of such evolved residual with more primitive magma forming the main stage of the filling history may have played a pivotal role in sulphur saturation and Ni-Cu-PGE scavenging. The work carried out on the mineralized Contact Breccia supports such complex magma mixing as might occur if dense residual collecting below Marginal Anorthositic Gabbronorite zones were still largely liquid when the main heave of primitive magma occurred, i.e. an early very high temperature (1300°C) and crustally-contaminated melt capped the rising magmatic stems feeding the individual EBL centers. The main magma chambers developed immediately above where such stems were choked off from further advance by high temperature plagioclase crystallization and this occurred at relatively shallow crustal levels where magmatic pressures equaled the lithostatic load. In such a case, the top of the conduit, between capping anorthositic mush and sidewalls would be infiltrated when the main chamber was flooded, providing a setting for wholesale magma mixing within Contact Breccia. Commingled melt formed pyroxenitic pegmatoid between Marginal Leucogabbronorite and overlying Olivine Gabbronorite at the base of the Layered Series. Given the local size of basement blocks (1-1 Om scale) and mega-rafts (10-100m scale at Azen)) of basal Layered Series within the Contact Breccia, it is likely that the main RVI chamber was essentually fed by sidewall magma conduits and the chamber grew essentially by subsiding into its own conduit.
The Layered Series documents an episodic filling history whereby some operative fault valve pressure release mechanism, balancing hydrostatic pressures and the increasing lithostatic load, controlled the magma supply. These discrete magma pulses differentiated from olivine rich bases, through oikocrystic bronzitite centers, to plagioclase rich tops. m the RVI, these individual magma pulses give rise to thick 30 to 50 meter thick fractionated units locally characterized by internal layering at the decimeter to meter scale, probably driven by internal convective turnover within given magma pulses. It seems likely that in the RVI, the Layered Series and overlying Upper Series have connected crystallization histories, with the unlayered Leucogabbro Zone at the base the Upper Series developing through continuing floatation of plagioclase throughout the filling history of the Main Layered Series. The occurrence of coarse amoeboid olivine lenses within the uppermost part of the Marginal Anorthositic Gabbronorite Zone indicates magmatic overpressures leading up to the development of the main chamber permitted limited seepage of primitive melt into the fractionated plagioclase rich mush, part of which may have delaminated to cap the main chamber. Sulphur saturation may have been attained in the pegmatoidal Transition Zone separating Layered Gabbronorite and Upper Leucogabbro through mixing residual oxide melt ponding below Upper Leucogabbro with the latest and most evolved magmatic pulses released into the main chamber. Such a history might account for the significant shift in metal ratios between basal contact-type ores and upper reef-type enrichments in the Transition Zone: contact ores are richer in Ni and Pd and have a Pd/Pt ratio about 3; Transition mineralization is rich in Cu, lower in Ni-Pd tenor, and has a Pd/Pt ratio about In addition to significant evident variation in primary magmatic Ni-Cu-PGE signatures, there is considerable evidence to indicate that Grenville mylonitic shearing and amphibolitic recrytallization caused dramatic secondary remobilization of primary sulphide. The retrograde mylonitic shears with associated chlorite at Dana have associated enrichment in As, suggesting these are especially effective sinks for low temperature (350°C) hydrothermal mineralization. The gametiferous shears developed at amphibolite facies conditions have associated barren pyrite. likely the direct result of these shears being conduits for wholesale metamorphic desuphidization. The pervasively recrystallized part of the RVI south of the Sturgeon River Fault may entirely lack primary magmatic sulphide ores, as it is so far known to be host to only prospects rich in secondary Cu more or less devoid of any associated Ni-PGE enrichment.

References
Note that most of the age dates quoted through this report can be found in Table 3 of Easton, R.M., Jobin-Bevins, L.S., and James, R.S. 2004. Geological guidebook to the Paleoproterozoic East Bull Lake intrusive suite plutons at East Bull Lake, Agnew Lake and River Valley, Ontario; Ontario Geological Survey, Open File Report 6135, 84p.]]> Maps 0 1 Lat-Long coordinates 0 57E,65N 0 -80.2677143927381 46.64270577728772 0 5749.936603770406 0 -3.012703292300555 #sn_icon63_copy28 -80.25483850369041,46.63587696503267,0 56E,73N 0 -80.26345141107178 46.70828746333608 0 2724.148490675399 3.0534500699944e-012 -3.009753579776912 #sn_icon63_copy27 -80.26702654288346,46.70815851054023,0 56E.72N 0 -80.26751161858196 46.699489679704 0 1011.567342510325 0 0.006571846684246555 #sn_icon63_copy25 -80.26758417831212,46.69921970471101,0 55E, 73N 0 -80.27925997284578 46.70314959015173 0 1892.900752962793 0 -0.001978571528041432 #sn_icon63_copy24 -80.28017762639954,46.70810187856624,0 54E,72N 0 -80.28186467778122 46.70370278016899 0 2727.112958740542 1.515264273978634e-011 -3.023154392562621 #sn_icon63_copy32 -80.29366826207604,46.69988500832368,0 Total Magnetic Field 0 http://instruct.uwo.ca/earth-sci/fieldlog/Sudbury/Total%20Magnetic%20Field.jpg 0.75 46.99375276144443 44.44030358042292 -79.31043152760815 -81.99476097030096 -0.07824263839759266 Kelly, Davis, McNish, Janes Townships - Geology 0 http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/Kelly_Davis_McNIsh_Janes_tnshps.jpg 0.75 46.7486984551901 46.65556304983964 -80.31194782815911 -80.499613998407 -0.01097156998608152 Dana North Property 0 Field Guide http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/River_Valley.doc 1 http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/Dana%20North.jpg 0.75 46.70883590918959 46.6963403573594 -80.26720820472146 -80.28123787726072 River Valley 0 http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/river_valley3453.jpg <> Legend for the Glen Afton (River Valley) map http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/rvlegend.jpg]]> http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/river_valley3453.jpg 0.75 46.76117952396906 46.63173578460584 -80.20291597758204 -80.34479754305988 -0.6828750027810289 Sudbury diabase 0 -80.26472489230072 46.66873426664379 0 8033.497845957012 2.647784697775263e-012 0.01823839997468606 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy63 -80.26359292059907,46.6798595728974,0 Sudbury diabase 0 -80.26472489230072 46.66873426664379 0 8033.497845957012 2.647784697775263e-012 0.01823839997468606 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy66 -80.2399958850569,46.6606927198428,0 Textural Preservation Map 0 5 http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/Easton03textpres.jpg 0.75 46.72573686266526 46.52681943263309 -80.06281249628108 -80.31147242944087 SEG Field excursion November 2007 0 Stops taken from various published field guides 0 1 Warren to River Valley 0 1 Syenite pegmatite quarry 4.8 km 0 -80.28192892966243 46.46015292657646 0 9198.302388607861 1.651864558934176e-012 0.2914361548979531 relativeToGround #msn_ylw-pushpin_copy1 -80.28937686764392,46.47663326474432,0 FTG06 stop 1A Crerar Gneiss Association 14.5 km 0 -80.26315010773742 46.55265982514347 0 4218.280439495099 4.894846084738729e-012 0.1368835498387973 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy57 -80.26859330590456,46.55139401546068,0 FTG06 stop 2A Crerar gneiss megacrystic granite 21.6 km 0 -80.19068534557668 46.57081755387717 0 6559.26366771474 0 0.05261722438991574 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy58 -80.19192338162083,46.56468798780808,0 Crerar gneiss assocation 12.5 km 556236E, 5153510N NAD83 0 -80.27364770257961 46.52409873186088 0 10805.25263353121 5.05620697723434e-012 0.2974387267431746 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy62 -80.26663047185517,46.53283166788958,0 Sturgeon Falls to River Valley 0 1 FTG06 stop 1B Crerar gneiss assoc 2.2 km out of Field 0 -80.05442108626831 46.52780426712682 0 1221.34466889494 0 0.2132671879108476 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy53 -80.05551790454229,46.52716416796126,0 FTG06 stop 2B Crerar gneiss megacrystic granite 11.1 km from Field 0 -80.14535241305867 46.5652893082809 0 1293.819697541921 1.593175448658762e-011 0.147268899448032 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy54 -80.1459740723981,46.56483173880114,0 Stops related to the geology of the River Valley region 0 1 FTG06 stop 3 Red Cedar Lake gneiss 0.0 km 0 -80.18009462574997 46.57777780298921 0 2695.548162696288 0 0.1221580945181316 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy56 -80.17673877500451,46.57702602011976,0 Junction of 539A and 805 to west 0 -80.21709223153687 46.6173593466696 0 834.2496422046351 0 0.09518946732897317 relativeToGround #sn_icon63_copy300 -80.2169429482163,46.61794170557434,0 FTG06 Stop 4 Varied degrees of preservation in rocks of the River Valley intrusion 6.2 km 559691E, 5163308N WGS84 0 -80.21709223153687 46.6173593466696 0 1532.780387471905 0 0.09518946732896999 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy49 -80.22047310200378,46.62045330385697,0 Dana1, Varley 0 -80.22907322068156 46.66536789533476 0 7027.011816443702 1.422627877247619e-012 0.06616048279433298 relativeToGround #msn_icon63_copy37 -80.2380260570895,46.66132341503942,0 FTG06 Stop 5 Autolith fragments and layering, Layered gabbronorite zone 13.6 km 0 -80.2345938256211 46.65978647752582 0 2912.082048195627 0 0.06214584451091228 relativeToGround #msn_icon63_copy49 -80.23939416083681,46.66034262297179,0 FTG06 Stop 6 Layered Olivine gabbronorite 15.7 km 559446E, 5166397N WGS84 0 -80.22047246443405 46.65653515939535 0 2083.924572195168 9.89255130341834e-012 0.09274285379248691 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy59 -80.22301429195372,46.65750058537594,0 Turn off 805 onto gravel logging road ?? 9 km 0 -80.24737995552999 46.63649658069857 0 3149.747981806474 0 0.05284879283502317 relativeToGround #sn_icon63_copy41 -80.25201442129335,46.63475120333045,0 FTG06 Stop 7 Footwall alkali feldspar granite and FTG06 Sudbury diabase dike 17.5 km 559785E, 5167228N WGS84 0 -80.21646923136862 46.65644064309289 0 2854.332979680837 0 0.04373353692760836 #msn_icon63_copy29 -80.21861944444444,46.65594166666666,0 FTG06 Stop 8 Azen Creek Cu-Ni-PGE occurrence 18.2 km 0 -80.23096872823884 46.6562410571143 0 5239.341804751046 0 0.06478053837859246 relativeToGround #sn_icon63_copy31 -80.22724715248464,46.65865832474571,0 FTG06 stop 9 (Lumbers 1978, stop 2.6) Huronian Metavolcanic rocks 0 -80.2937029452649 46.64735784327357 0 683.5488997951509 5.052876704810967e-013 0.0394945651910324 relativeToGround #sn_icon63_copy53 -80.2943304709118,46.64736548157123,0 FTG06 stop 10, 7.6-8.1 km) Nipissing gabbro 0 -80.27772676946042 46.66698599262496 0 3380.857567292961 4.269180952276323e-012 -3.019379509276811 relativeToGround #sn_icon63_copy36 -80.28392460337881,46.66791148457137,0 FTG06 stop 11 mylonitized RV anorthosite 0 -80.28340582142344 46.67140777509361 0 2152.063225742235 0 0.02647395208084716 relativeToGround #sn_icon63_copy54 -80.28673226556199,46.66787159784444,0 Protomyl. leucogabbro intruded by def. felsite veins (FTG 8.4-8.6 km) 0 -80.28124721946821 46.67062082507255 0 3320.627801559962 0 0.02804458448238342 relativeToGround #sn_icon63_copy38 -80.28824772903741,46.67106292095746,0 FTG stop 12 mylonitized anorthosite of the RV intrusion 9.3 km 0 -80.28148240856959 46.68113239789755 0 3320.62780156067 9.396409440545106e-012 0.0278739568239716 relativeToGround #sn_icon63_copy48 -80.28931828604698,46.67798368026842,0 FTG06 Stop 13 FTG06 NIpissing Gabbro and mylonite 9.5-9.7 km 554175E, 5169990N WGS84 0 -80.28158635154072 46.68120377709798 0 3320.627801559962 0 0.02779834379458682 relativeToGround #sn_icon63_copy40 -80.29132710399318,46.68102824357556,0 FTG06 stop 15 Mississagi Fm and mylonitic contact with the RV554413, 5172600, east = deformed Mississagi Fm.; 0 -80.28420635811158 46.69763746568336 0 3068.845815424804 0 -3.022618312636508 relativeToGround #sn_icon63_copy45 -80.28817847900784,46.70475628155435,0 FTG06 stop 14 west = Gowganda? conglomerate; east = ultramylonite 0 -80.2836776090702 46.6828584427736 0 3092.402752266793 0 -3.022235686935717 relativeToGround #sn_icon63_copy44 -80.29313626285149,46.6836577622985,0 FTG06 Stop 16 Mississagi Fm 15.1 km 0 -80.29252291686552 46.72513148046772 0 4259.412476667603 2.510257117465071e-012 0.01983524117263951 relativeToGround #sn_icon63_copy52 -80.29052224190092,46.72176021366153,0 FTG06 stop 17 Gowganda Fm 17.5 km 552600E, 5176075N WGS84 0 -80.30380534746249 46.7334121339341 0 2152.063225745064 0 0.01162332784723806 relativeToGround #sn_icon63_copy46 -80.31149559893061,46.73614869738546,0 Miscellaneous stops 0 1 Stop 9 Dana Lake Cu-Ni-PGE occurrence 0 -80.2710178626369 46.70207722924138 0 2785.179759709564 0 -3.01272595881329 relativeToGround #sn_icon63_copy20 -80.27591856736211,46.7047264518322,0 mylonite sep. Mississagi from foliated RV leucog 0 -80.28420462830306 46.69761499433376 0 3068.782495403532 2.06487749863257e-012 -3.022617053778144 relativeToGround #sn_icon63_copy23 -80.2856580176949,46.70488301934547,0 Stop 8b (FTG06 stop 15) Mississagi Fm and mylonitic contact with the RV554413, 5172600, east = deformed Mississagi Fm.; 0 -80.28420635811158 46.69763746568336 0 3068.845815424804 0 -3.022618312636508 relativeToGround #sn_icon63_copy50 -80.28817847900784,46.70475628155435,0 Stop 8 RV mylonitized anorthosite 0 -80.28187845588016 46.67788423297476 0 3073.484876326881 8.042986675551033e-012 -3.020927302971742 relativeToGround #sn_icon63_copy12 -80.28813760322578,46.67621548258963,0 RV varitextured gabbro (FTG 8.7 km 554500E, 5169105N WGS84) 0 -80.28124721946821 46.67062082507255 0 3320.627801559962 0 0.02804458448238342 relativeToGround #sn_icon63_copy43 -80.2874146257812,46.67327437145939,0 7c (FTG stop 10, 7.6-8.1 km) Nipissing gabbro 0 -80.27772676946042 46.66698599262496 0 3380.857567292961 4.269180952276323e-012 -3.019379509276811 relativeToGround #sn_icon63_copy39 -80.28392460337881,46.66791148457137,0 7b-2.5 - gneissic leucogabbro 0 -80.28736339897932 46.6598881754641 0 3387.219960302161 0 -3.026389301428041 relativeToGround #sn_icon63_copy18 -80.27717451144117,46.66420380765458,0 7b-1-1.2 West=mafic Huronian metavolc; east = RV leucog. 0 -80.28832241551034 46.65485753366484 0 3413.678366316948 0 -3.027086809212841 relativeToGround #sn_icon63_copy17 -80.2865066720845,46.65441186459026,0 Stop 7b (FTG06 stop 9; Lumbers 1978, stop 2.6) Huronian Metavolcanic rocks 0 -80.2937029452649 46.64735784327357 0 683.5488997951509 5.052876704810967e-013 0.0394945651910324 relativeToGround #sn_icon63_copy35 -80.2943304709118,46.64736548157123,0 7-0.3 0 -80.2146204593256 46.61867874111638 0 8334.259725034053 0 -2.973518449303634 relativeToGround #sn_icon63_copy7 -80.22154662169828,46.6206664815759,0 7-5.4 0 -80.23240962569768 46.63103332944236 0 9935.311968895239 1.538479054891926e-012 -2.98644309612677 relativeToGround #sn_icon63_copy9 -80.27450836682534,46.64032129575071,0 Locations other than stops 0 1 Varley 0 -80.22400251485269 46.64565040157417 0 4455.919376821609 0 0.03825657649578985 #khStyle806000 -80.23866666666666,46.66672222222222,0 River Valley 0 -80.17684256280441 46.59644378138832 0 12395.06875145663 0 -2.946596242299068 #msn_icon63_copy11 -80.18233007649099,46.58665181706622,0 Erana Mine rd 0 -80.19681332500295 46.6128297290587 0 8283.93197324315 0 -2.960580024206215 relativeToGround #sn_icon63_copy26 -80.19903506999947,46.60684551196794,0 Erana Quarry 0 -80.15994102338266 46.62274178147005 0 2300.518503975544 0 0.08480467243954862 #khStyle81800000 -80.16414052256479,46.62463796208842,0 Road to Azen creek 0 -80.21555077782203 46.61942681415899 0 2784.103488814071 1.190368819369864e-011 -2.974194654928172 relativeToGround #sn_icon63_copy13 -80.21629851979208,46.61787337779535,0 Azen Zone 0 -80.22400251485269 46.64565040157417 0 4455.919376821609 0 0.03825657649578985 #sn_icon63_copy4 -80.22727777777777,46.65972222222222,0 Thompson 0 -80.23442749377023 46.64151779720351 0 3149.747981807888 0 0.06226474042960518 relativeToGround #sn_icon63_copy33 -80.23419583784262,46.64256655184662,0 Glen Afton 0 -80.28163803556897 46.64992569841413 0 5732.407887730196 1.324984443880865e-011 -3.022825741949538 #khStyle9060012 -80.29492714292098,46.64665864512428,0 Jackson Flats 0 -80.1959564965848 46.65669411542802 0 4571.35450807659 8.90914831979185e-012 0.05862197394829803 #sn_icon63_copy6 -80.19768348141531,46.6584920794221,0 Dana Garnet 0 -80.19198418679343 46.63055693134796 0 11773.47789396302 1.369042082804264e-011 0.06153377444522731 #khStyle81800000 -80.18747499767299,46.66835347684504,0 Dana Quarry 0 -80.23442749377023 46.64151779720351 0 3149.747981807888 0 0.06226474042960518 relativeToGround #msn_icon63_copy34 -80.23212796640468,46.64127920372841,0 Cre-mac 0 -80.16852713502412 46.63166204177851 0 4529.107261847079 8.909113575860791e-012 0.07856453642210119 #khStyle81800000 -80.17776265607007,46.63600825737007,0 Turn off to Pacific NW Cap. Corp Dana North 0 -80.28035557832506 46.70675912114217 0 3072.767112454508 0 -3.01981555595503 relativeToGround #sn_icon63_copy16 -80.28335134565828,46.70870556394167,0 Links to documentation 0 Stops SEG 2007 field excursion - Parry Sound to Kirkland Lake 0 Parry Sound motel 0 -80.00083371740998 45.3402100720244 0 313.7872417075426 12.86922691099022 -3.032325276397464 relativeToGround #msn_donut -80.00130398422863,45.34002132126125,0 Parry Sound gabbroic anorthosite shear pod 0 -80.02188071447239 45.36507478969745 0 269.3210287472934 12.86918107894543 -3.047299619344396 relativeToGround #msn_donut_copy0 -80.02250822364384,45.36506941952824,0 Parry Sound, extensional structures 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Parry_Sound/PS_extena188.JPG <> Close-up of above structure <> http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Parry_Sound/PS_extenb189.JPG <> Coronitic reaction rim around garnet porphyroblast <> http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Parry_Sound/PSgarnet186.JPG <> Amphibole-filled extension fracture in a metagabbro shear pod within amphibolitic schist (Bottom right) <> http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Parry_Sound/PSext_crcka184.JPG <> Tourmaline in extension fracture <> http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Parry_Sound/PS_tourm183.JPG<>]]> -80.01863028085882 45.36282568061201 0 285.2210405297554 12.86921292384985 -3.044986705353027 relativeToGround #msn_donut_copy25 -80.01853573971536,45.36304545406052,0 001 Key River 0 #msn_donut_copy00 -80.56556200000001,45.892482,177.968384 002 0 #waypoint0_copy0 -80.581069,45.95161000000001,202.001221 003 0 #waypoint0_copy0 -80.57180900000002,45.979632,189.263916 004 0 #waypoint0_copy0 -80.573116,46.007045,208.249756 005 French River 0 #msn_donut_copy1 -80.584315,46.019811,198.39624 006 0 #waypoint0_copy0 -80.62106799999999,46.05266600000001,185.178223 007 Rutter 0 #msn_donut_copy2 -80.66663100000001,46.104442,206.567505 008 Jamot 0 #msn_donut_copy3 -80.57452000000001,46.100171,199.5979 009 Quartzite 0 #msn_donut_copy4 -80.56345500000001,46.10583100000001,200.078613 010 Noelville 0 #msn_donut_copy5 -80.431696,46.13722200000001,220.987183 011Foliated meta-gabbro 0 #msn_donut_copy6 -80.43288,46.24400300000001,215.219238 012 St Charles anorthosite-metagabbro, plag megacrysts 0 #msn_donut_copy7 -80.415144,46.36216200000001,221.227539 Hagar, jnctn 535 and 17 0 -80.41757389525098 46.45323388936738 0 4872.792347109725 0 -0.001798569749289783 relativeToGround #msn_ylw-pushpin10 -80.41608234664672,46.45491707956994,0 012ASturgeon Falls 0 -79.92233763157573 46.36876418534624 0 16235.09492941848 12.86922691098977 -2.9730360708394 relativeToGround #msn_ylw-pushpin01 -79.9294815000064,46.36615177289821,0 Field - Val des Arbres, jnctn 64 and 539 0 -80.03530012038749 46.52512000287877 0 4069.948691143861 0 -0.05014095805427895 relativeToGround #msn_ylw-pushpin -80.02862307511622,46.52500472634028,0 013 River Valley 0 #msn_donut_copy8 -80.182703,46.586756,242.135986 014 Bridge 0 #msn_donut_copy90 -80.189545,46.596669,243.09729 015 road crosses railtrack 0 #msn_donut_copy10 -80.226467,46.623224,241.414917 016 sharp bend in the road 0 #msn_donut_copy11 -80.264955,46.641777,238.771362 017 Glen Afton 0 #msn_donut_copy120 -80.29406899999999,46.648312,242.135986 018 Stop 1 complex contact facies of the River Valley complex with the Pardo paragneiss unit 2d 0 http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/RV191.JPG
Contact of mafic and leucocratic facies of the River Valley complex marginal breccia
http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/RVa190.JPG
Amphibole 'combs' in heterogeneous gabbro - rusty areas reflect the presence of PGE-bearing sulphide patches
http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/RVc192.JPG
Pegmatoidal patch (worm intrusion?) within leucocratic block in amphibolitic schist
http://instruct.uwo.ca/earth-sci/fieldlog/River_Valley/RVd2_194.JPG
]]> #msn_donut_copy27 -80.276438,46.707285,326.731323 019 Stop 2 large well exposed outcrops of River Valley gabroic anorthosite of the "Marginal Breccia" unit 0 #msn_donut_copy29 -80.276505,46.704618,316.156982 020 rd leading to the Dana North Prospect 0 #msn_donut_copy26 -80.27824500000001,46.70974600000001,277.704468 021Gowganda 0 #msn_donut_copy13 -80.291363,46.681372,305.822876 022 Marten River, jnctn 11 and road from Field 0 #msn_donut_copy16 -79.811477,46.75015300000001,292.364502 023 Archean Granitic rocks 0 #msn_donut_copy17 -79.80795500000001,46.76690800000001,296.209717 024 Temagami Gowganda unconf. on Timiskaming 0 #msn_donut_copy18 -79.79683300000001,47.05679,314.234253 025 Temagami Busy Bee restaur. 0 #msn_donut_copy19 -79.789361,47.063579,323.366699 028 Jnctn of 11 and 11B into Cobalt 0 #msn_donut_copy22 -79.759084,47.375865,353.407715 029 Cobalt lamprophyre dike 0 #msn_donut_copy23 -79.676154,47.394147,337.0654300000002 030 Start point of Cobalt tour 0 #msn_donut_copy24 -79.678641,47.395533,313.032593 031Bend 624 outcrops 0 #msn_donut_copy210 -79.7007318115235,48.00258618021942,311.830933 032 Misema River 0 #msn_donut_copy20 -79.768169,48.106227,321.9248050000002 Sudbury 0 1 Maps 0 Sudbury - geological map 0 http://instruct.uwo.ca/earth-sci/fieldlog/Sudbury/sudbury072048.jpg 0.75 46.90945536627419 46.29515148858012 -80.58846996561985 -81.66836356092942 0.2940282245465303 Total Magnetic Field 0 73ffffff http://instruct.uwo.ca/earth-sci/fieldlog/Sudbury/Total%20Magnetic%20Field.jpg 0.75 46.99375276144443 44.44030358042292 -79.31043152760815 -81.99476097030096 -0.07824263839759266 Coniston_Garson_Falconbridge 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Sudbury/2491falconimage.jpg 0.75 46.58364103612666 46.42206006496645 -80.75414600036201 -80.89578452950084 Rathbun Township 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Sudbury/2491rathbun.jpg 0.75 46.84272294156159 46.68016027161821 -80.61534908177949 -80.75744700986883 Parkin_Aylmer Townships 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Sudbury/2491aylmer.jpg 0.75 46.8384601823652 46.74183732027142 -80.74562385132316 -80.98301723456791 -0.7205884258917832 Snider Township 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Sudbury/2491snider_1700.jpg 0.75 46.52972559811039 46.42455625292899 -81.02708337753828 -81.16548315648127 Scadding Township 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Sudbury/2491scadding.jpg 0.75 46.70742139204579 46.54416327872512 -80.6125670869685 -80.75245654924794 Huronian outliers north of Sudbury 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/outliers/huroutliersmap.jpg 0.75 46.95975149117524 46.37324589853347 -81.19311308149116 -81.85004473046074 0.03350923156825321 Ames - Ramsey Lake - Coniston region 0 ames_Coniston1_1.jpg 0.75 46.57466314963224 46.46468289777301 -80.7255991838577 -81.03777678365483 Ames - Kelly Lake 0 ames_Kelly1_1.jpg 0.75 46.46999741375841 46.41978100029292 -81.04209659846691 -81.11434041291965 Ames - Copper Cliff 0 ames_Copper1_1.jpg 0.75 46.52974775796789 46.46946157422118 -80.99977019668074 -81.10372496102346 Copper Cliff to Richard Lake 0 4 ames_S_Sud_1.jpg 0.75 46.48841231710849 46.39720396853728 -80.87425928238001 -81.10649298434545 North Range - Windy Lake_Levack 0 Maps 0 High Falls 0 2A - Micropegmatite and basal breccia.
Intermingled plagioclase-rich and granophyre-rich varieties are present ; neither shows chilled contacts. Gneiss inclusions derived from the basal breccia consisting of large/small basement fragments (metaseds, granites. gneiss) in a recrystallized pseudo-igneous matrix of quartz, albite, and chloritized anhedral mafic patches - pulverized rock fragments; some planar shock features persist notably in fragments that appear dark gray in colour.
2B - Micropegmatite basal breccia
lens of plag-rich micropegmatite intrudes basal breccia; stoped fragment of basal breccia complete with matrix is enclosed by the micropegmatite; contact is exposed a few feet north of the lens.
2C - Basal breccia and hornfelsic Gray Onaping

2D - Melt Rock and basal breccia
2E - Melt, basal breccia and quartzite
2F - Melt, chilled and chilled-brecciated melt; devitrified glass flows and Gray Onaping
]]> 5 High_Falls3_1.jpg 0.75 46.60177160363392 46.59528059809934 -81.38333838993789 -81.39254753689389 -3.780296689077318 HIgh Fall 1 0 4 High_Falls1_1.jpg 0.75 46.59940831864494 46.59248506985812 -81.3809651537636 -81.39030848353252 -1.522591746194766 High Falls 2 0 High_Falls2_1.jpg 0.75 46.60235046944239 46.59539353186894 -81.38700857085782 -81.39586980662396 -1.75834853200245 Windy Lake pseudotachylite (parking area) 0 -81.45823941252309 46.62771763862089 0 1606.383193933718 2.186660541141709e-011 -5.544891887825462 #default_copy:0_copy6400012000 -81.46163137269947,46.63095280794033,0 Windy Lake felsic norite 0 -81.42678906078223 46.61438675724875 0 1668.546165661949 5.157770044465309e-011 -5.522033208227659 #default_copy:0_copy65000002010 -81.42838512692461,46.61522202302758,0 Grey Onaping 0 -81.38174414605817 46.5981064387383 0 1803.720425102462 6.643428060073677e-011 -5.489301773701241 #default_copy:0_copy6700011021 -81.38278003663837,46.59747893866212,0 Melt breccia bedded clast 0 -81.38539737169809 46.59908227057543 0 1700.249314540949 6.64333621881462e-011 -5.491955845894639 #default_copy:0_copy6800101000 -81.3875,46.59836111111111,0 Granophyre 0 -81.38539737169809 46.59908227057543 0 1700.249314540949 6.64333621881462e-011 -5.491955845894639 #default_copy:0_copy69002004 -81.38874589684123,46.59910298553055,0 Levack granophyre in acicular amphibole 'diorite' (magnetite quartz gabbro) 0 -81.40944199595086 46.61774488979688 0 1587.840756782638 5.157707821556502e-011 -5.509425739564217 #default_copy:0_copy660000010 -81.41178130725324,46.61657704656304,0 HIgh Falls 0 -81.38037938662932 46.59078589385887 0 2602.453023613805 0 -0.8942634347013034 relativeToGround #msn_ylw-pushpin501 -81.38196053522488,46.59327747043915,0 Black Onaping w. melt fragments 0 -81.38037938662932 46.59078589385887 0 2602.453023613805 0 -0.8942634347013034 relativeToGround #msn_ylw-pushpin_copy11000 -81.38326018632925,46.5905729396311,0 Onwatin Slate 0 -81.30974384139854 46.58570798974667 0 2833.32683577659 0 -0.8419816299049014 relativeToGround #sn_ylw-pushpin0300 -81.3187337103183,46.58636297381694,0 Chelmsford greywacke 0 -81.28743342278307 46.57234270522239 0 738.2246574753771 0 -5.420818954826348 #default_copy:0_copy700010003 -81.2870701467252,46.57292126272345,0 Levack 0 -81.37518558490575 46.6340625643249 0 8869.459046570548 0 -0.4552502139424875 relativeToGround #msn_ylw-pushpin36 -81.38841761774995,46.64060515636025,0 South Range 0 1 Stop 4 - Discovery site 0 -81.04394194120231 46.52287979622435 0 5405.811736238814 0 0.2485130348314404 relativeToGround #msn_ylw-pushpin371 -81.05353298641397,46.52085326646769,0 Stop 5 Copper Cliff offset 0 quartz diorite, less than 200 feet wide at this stop; ore grade mineralization is confined to a zone within the dike or at one margin; outer part of the offset dike is finer grained than the interior, which includes the mineralized zone defined by an abundance of sulphide blebs and small, generally amphibolitic inclusions]]> -81.06874897641208 46.48620532321314 0 546.6620693462634 0 0.2305135272019953 relativeToGround #msn_ylw-pushpin451 -81.0692444812312,46.48618317195416,0 Stop 6 0 thinly beeded turbidite with well preserved flame structures; abundant small pseudomorphs after staurolite imports a reverse graded bedding .; small shatter cones point northwards.]]> -81.05700722960201 46.46829159434008 0 5405.811736238082 0 0.2390276465047105 relativeToGround #msn_ylw-pushpin461 -81.05959782456458,46.46806639729595,0 Stop 7 Sudbury breccia, Ramsay Lake and Pecors formations 0 large inclusions in the breccia; they are dioriented and well rounded by attrition; occasional exotic blocks of units below or above the Ramsay Lake and Pecors; scarce shatter cones in the the Ramsay Lake conglomerate -81.03680612998163 46.45521403901002 0 1924.237864763898 0 0.2536706388351089 relativeToGround #msn_ylw-pushpin391 -81.03914992243975,46.4551935639954,0 stop 8 0 Beds dip 60 Se;prominent current bedding show south facing; shatter cones are several feet in size; each cone has numerous parasitic partial cones; apical angle is about 90 degrees; stereographic projection shows that they have a strong preferred orientation , with conical axes lying in the plane of the bedding plane; the axes point northwards; cone surfaces are only exposed where they parallel the surface of the outcrop; on other surfaces the interesecting crescentric fractures impart a shattered appearance to the rock]]> -81.07412792317108 46.43128732478624 0 473.2831908987862 0 0.2266242489426276 relativeToGround #msn_ylw-pushpin471 -81.07220625875635,46.43231731234627,0 Skead 0 -80.74925399999992 46.666771 0 999.9999999984239 0 1.192708005548819e-014 relativeToGround #msn_ylw-pushpin37 -80.74925399999992,46.666771,0 Nairn 0 -81.56756330558234 46.33566789980333 0 20710.91112174993 0 -0.5937132258398172 relativeToGround #msn_ylw-pushpin28 -81.626126787068,46.32483534528507,0 Maps 0 Shattercone locations 0 Sudbury_shatter_cones_1.jpg 0.75 46.88800182570318 46.29920710147916 -80.67254192865244 -81.68972387495617 Abundant Staurolite 0 -81.04039100179882 46.50600472308098 0 962.3702290068246 9.350479662822928e-011 -0.1310986516626015 relativeToGround #msn_ylw-stars_copy152 -81.03883253668188,46.50669961758041,0 Creighton Granite 0 -81.07009993437956 46.48618322556271 0 962.3702290054099 5.138717050904766e-011 -0.152647171114495 relativeToGround #msn_ylw-stars_copy16200 -81.07170268049602,46.48594446661888,0 Trap Dike 0 -81.06621246194906 46.48173614469913 0 962.3702290068246 1.145636096877899e-010 -0.1498280298549469 relativeToGround #msn_ylw-stars_copy53 -81.06908800362714,46.48174215978882,0 Retrograde McKim, shatter cones, F2+F3 cleavage 0 -81.05951265415183 46.46912659291286 0 962.3702290068246 9.350479662822853e-011 -0.1449709108289204 relativeToGround #msn_ylw-stars_copy14200 -81.05934029813699,46.46806763055522,0 Brecciated McKIm 0 -81.05951265415183 46.46912659291286 0 962.3702290068246 9.350479662822853e-011 -0.1449709108289204 relativeToGround #msn_ylw-stars_copy4 -81.06107127489365,46.4688356568471,0 Maps 0 Offset dike - Cobalt St, Sudbury 0 850area_1.jpg 0.75 46.47186649659241 46.46763573816243 -81.07462823917574 -81.07820277771597 Azilda -Black Onaping and Grey Onaping Granophyre transition 0 -81.10773835489525 46.56159095064179 0 2321.744820155831 8.730803719713188e-012 5.152374415829334e-011 relativeToGround #sn_ylw-pushpin_copy:0_copy:0_copy742 -81.10989057349087,46.55960392116712,0 Matachewan dike - 495692, 5150438 0 -81.05607057388107 46.50715052015688 0 341.3325586817078 9.252958495837474e-011 -0.1397826833917218 relativeToGround #msn_ylw-pushpin_copy:0_copy5110 -81.05603655320913,46.50670192568605,0 Pillow lava - 495817.93, 5151326.34 0 -81.0540477847205 46.51462088939212 0 1135.034527808275 0 -0.1383153275789435 relativeToGround #msn_ylw-pushpin_copy:0_copy430 -81.0545254076459,46.51548851614425,0 2001 0 00map1_01stati Events 0 Exported from 00map1_01stati Events on 2008-04-25 normal #FEATURES_copy1 highlight #FEATURES_copy2 Features 0 1 <Null> 0 #FEATURES_copy0 -80.8063254122041,46.4963859484289,0 <Null> 0 #FEATURES_copy0 -80.8063254122041,46.4963859484289,0 <Null> 0 #FEATURES_copy0 -80.8063254122041,46.4963859484289,0 <Null> 0 #FEATURES_copy0 -80.8063254122041,46.4963859484289,0 <Null> 0 #FEATURES_copy0 -80.8063254122041,46.4963859484289,0 <Null> 0 #FEATURES_copy0 -80.8096648243978,46.5028982337148,0 <Null> 0 #FEATURES_copy0 -80.80633878095841,46.5073024295306,0 <Null> 0 #FEATURES_copy0 -80.8278246663904,46.50964967107951,0 <Null> 0 #FEATURES_copy0 -80.8235853710532,46.5146109557967,0 <Null> 0 #FEATURES_copy0 -80.8200208055674,46.5124095162513,0 <Null> 0 #FEATURES_copy0 -80.82030075968839,46.5144798494207,0 <Null> 0 #FEATURES_copy0 -80.8303422279991,46.5090504636096,0 <Null> 0 #FEATURES_copy0 -80.83732831763111,46.50919560525511,0 <Null> 0 #FEATURES_copy0 -80.8375779307227,46.5085389934237,0 <Null> 0 #FEATURES_copy0 -80.8303989285745,46.50758362223031,0 <Null> 0 #FEATURES_copy0 -80.8525397747146,46.47541385102641,0 <Null> 0 #FEATURES_copy0 -80.8445462619793,46.533180369221,0 <Null> 0 #FEATURES_copy0 -80.84682038162271,46.5313655371676,0 <Null> 0 #FEATURES_copy0 -80.8557917978803,46.5313771989472,0 " (north of the rail tracks)" 0 #FEATURES_copy0 -80.8100887481142,46.48969658057041,0 " (this value is off by 1 km due to influence of the power line??) outcrop east side of the road at the power line" 0 #FEATURES_copy0 -80.85351717807311,46.5189369782109,0 "" 0 #FEATURES_copy0 -80.82137167574589,46.49398055326921,0 "(near railway), fine grained, rounded biotite-qtz-feldspar boulders, imbricated towards the west (Current?); E-W strike with relatively shal 0 #FEATURES_copy0 -80.8134134889854,46.5005105288303,0 "(west end of a small black outcrop); 15m wide cross cutting dike of Sudbury diabase striking 268" 0 #FEATURES_copy0 -80.8216340294854,46.4934499882882,0 "?" 0 #FEATURES_copy0 -80.88507125020691,46.467207531815,0 "20 degree contact between sandstone (west) and Nipissing gabbro (east)" 0 #FEATURES_copy0 -80.8371901506216,46.50744949742251,0 "agmatites with some bands of spotted (cordierite?) hornfels" 0 #FEATURES_copy0 -81.049003504765,46.51641041081041,0 "amphibolitized gabbro with patches of epidosite cut by pink granite that has suffered subsequent brittle deformation; 0 #FEATURES_copy0 -80.99964870018179,46.41069347135141,0 "Augen granite of the Creighton pluton" 0 #FEATURES_copy0 -81.0691068326876,46.4866025159102,0 "Balsam St intersection with highway 17; staurolite bearing meta-greywackes (turbidites); small shatter cones pointing 352 upwards" 0 #FEATURES_copy0 -82.101877106039,46.463766232952,0 "buff to pink weathering intermediate dike with small amphiolite needles; intrusion post-dates the regional shear deformation (foliation) see 0 #FEATURES_copy0 -81.0105283889289,46.4231935499536,0 "centre of bridge of highway" 0 #FEATURES_copy0 -80.8797051940189,46.4849132123792,0 "contact 030 between sandstone and Sud breccia" 0 #FEATURES_copy0 -80.885456908278,46.469628812343,0 "contact between Nipissing gabbro and 5 metre intermediate dike with amph. needles and garnet" 0 #FEATURES_copy0 -80.8218387181014,46.514563250988,0 "contact of fine grained Nipissing diabase and x-bedded sandstone" 0 #FEATURES_copy0 -80.8471675548427,46.50986614128,0 "contact of sandstone (with pyrrhotite) and Nipissing gabbro" 0 #FEATURES_copy0 -80.831767402976,46.50762164128721,0 "contact striking 110 between Nipissing gabbro and sandstone" 0 #FEATURES_copy0 -80.82474564604421,46.51458574076892,0 "contact with folded amphibolitic metagabbro" 0 #FEATURES_copy0 -82.09297378577541,46.2103518971402,0 "crenulation (148/90) wraps the staurolite in schists at the side of the road 0 #FEATURES_copy0 -81.0074145223154,46.3973556678727,0 "crossbedded" 0 #FEATURES_copy0 -80.81079794623101,46.4880868321566,0 "cut by Sud breccia' 0 #FEATURES_copy0 -80.82234561901632,46.51502301555,0 "deformed Sudbury breccia; granite sill in Mississagi Sandstones; highway to Long Lake" 0 #FEATURES_copy0 -81.01057987248871,46.42023265126619,0 "diabase either intruding or a clast in breccia; strike 120; dikelets cross cut Nipissing at 513642, 5148727" 0 #FEATURES_copy0 -80.8212482370638,46.4918834612623,0 "dike 010/64 of plag, amph-needles, garnet + Sud Breccia, shatter cones; bedding 184/74" 0 #FEATURES_copy0 -80.81883017300849,46.49019673717991,0 "downward pointing shatter cone locality near Anderson Lake 0 #FEATURES_copy0 -81.86492260291681,46.2207648989612,0 "drill site 267" 0 #FEATURES_copy0 -80.82535137672301,46.512687765452,0 "fold plunge 54/52 varying from 188/58 to 275/60" 0 #FEATURES_copy0 -80.8539428059911,46.47684658655621,0 "fold structure beds varying in orientation from 30/82 to 111/78; plunge 341" 0 #FEATURES_copy0 -80.8518495912147,46.475331962785,0 "folding Sud breccia" 0 #FEATURES_copy0 -80.85290247915719,46.47617028392621,0 "folding from 102/67 to 210/84 plunge east" 0 #FEATURES_copy0 -80.8533048061949,46.47672877537571,0 "folding from 217/85 (north limb) to 93/68 and back to 34/80" 0 #FEATURES_copy0 -80.8529812934995,46.475927396243,0 "foliated amphibolite likely Nipissing gabbro cutting distal greywackes now crenulated garnet-mica schist; foliated rocks and D2 folds are cu 0 #FEATURES_copy0 -82.46208263546382,46.1996834582921,0 "foliated Sudbury breccia" 0 #FEATURES_copy0 -80.88508595476981,46.47259830838681,0 "Garson Road, contact 343/50 between Sud breccia and sandstone" 0 #FEATURES_copy0 -80.8325523166309,46.51093462415831,0 "Garson Road, contact strike 164 of Nipissing and Sudbury breccia" 0 #FEATURES_copy0 -80.83355298569781,46.51192603379841,0 "Garson Road, contact strike 164 of Nipissing and Sudbury breccia" 0 #FEATURES_copy0 -80.8331119655315,46.5112144277395,0 "Garson Road, dike trending E-W" 0 #FEATURES_copy0 -80.83508390064981,46.51001134955801,0 "Garson Road, folds, with near horizontal axes, verging west" 0 #FEATURES_copy0 -80.8318123781572,46.5099435892511,0 "Garson_Coniston area" 0 #FEATURES_copy0 -80.819259658896,46.5100144388795,0 "Garson_Coniston area, Contact, strike 303, of Nipissing and sandstone; abundant cleaved Sudbury Breccia" . 0 #FEATURES_copy0 -80.80859607458932,46.5066222635592,0 "Garson_Coniston area, felsic dike with acicular amphibole 256/80" 0 #FEATURES_copy0 -80.80792916830261,46.4961366649549,0 "Garson_Coniston area, felsic dike with acicular amphibole 256/80" 0 #FEATURES_copy0 -80.80792916830261,46.4961366649549,0 "Garson_Coniston area, hill on the pipe line track on way out to the Garson Road" 0 #FEATURES_copy0 -80.82656840706081,46.50710090263991,0 "Garson_Coniston area, irregular felsic dike app. strike 244" 0 #FEATURES_copy0 -80.8063254122041,46.4963859484289,0 "Garson_Coniston area, lunch stop" 0 #FEATURES_copy0 -80.8063254122041,46.4963859484289,0 "Garson_Coniston area, view of anticline cut at the top by an E-W mafic trap dike strike 284; 0 #FEATURES_copy0 -80.8168348082483,46.5101275756952,0 "high strain zone in granite" 0 #FEATURES_copy0 -81.0490037879115,46.51672539416351,0 "highly (rutiliferous) 50 m wide altered Loon Lake fault zone (8786) separating the North and South deformation domains" 0 #FEATURES_copy0 -81.725926498845,46.20712496450721,0 "Hydro road junction with 17 east of Sudbury water works; travnum (col 4) 1 = wrc; 2 = krista; 3 = theresa; 4 = maria; 5 = grant 0 #FEATURES_copy0 -80.8154367445803,46.48800441559051,0 "isoclinally folded metasediments intruded by foliated granite; near small lake" 0 #FEATURES_copy0 -80.96891533266762,46.3897919170397,0 "Junction of Landing road and the Deer Lake Road" 0 #FEATURES_copy0 -80.73904992450829,46.4050949341801,0 "junction of road and side road on south side of the railway tracks" 0 #FEATURES_copy0 -80.88022658141961,46.4848057645946,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_copy0 -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_copy0 -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_copy0 -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_copy0 -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_copy0 -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_copy0 -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_copy0 -80.7564508864801,46.4152399783552,0 "location of bridge south of the pumping station" 0 #FEATURES_copy0 -80.8383803806521,46.5104570322177,0 "McKim turbidites; chloritoids wrapped in S2 foliation predate the main foliation" 0 #FEATURES_copy0 -81.77855709743029,46.2713716484479,0 "Murray Mine plaque; south along the rail track one encounters aphyric and plag-phyric mafic units pink granite, grey monzodiorite/granodio 0 #FEATURES_copy0 -81.05203248981169,46.5211878205103,0 "Nipissing gabbro" 0 #FEATURES_copy0 -80.88781530472291,46.46921716811571,0 "Nobel eclogite? Body" 0 #FEATURES_copy0 -80.10523404759761,45.4233110981542,0 "outcrop west of rail track before the bend approaching Coniston; Sudbury breccia but some beds possibly striking 280" 0 #FEATURES_copy0 -80.843312512071,46.49966443759261,0 "Outcrops of X-bedded sandstone at the western margin of the Nipissing diabase east of the Garson road to the south of the gravel quarry; Z-f 0 #FEATURES_copy0 -80.8391564417164,46.499244689306,0 "outcrops with large staurolite xls; on east side of the road are beautifully preserved soft sedimentary structures (sheath-like folds); thes 0 #FEATURES_copy0 -81.04913824926931,46.50680784843921,0 "pegmatite spiral in Nipissing" 0 #FEATURES_copy0 -80.8420472719109,46.5360387871656,0 "photograph of metasandstone with a shatter cone and blebs" 0 #FEATURES_copy0 -80.8637859731757,46.5154398514212,0 "Point zero at road side " 0 #FEATURES_copy0 -80.8433617701279,46.5324227950819,0 "Red Deer Lake agmatite, south side of road" 0 #FEATURES_copy0 -80.732196754651,46.4044851105813,0 "Red Deer Lake, Sudbury diabase north side of road" 0 #FEATURES_copy0 -80.732183745165,46.404485080116,0 "Red Deer Lake, Sudbury diabase outcrop north side of road" 0 #FEATURES_copy0 -80.732196754651,46.4044851105813,0 "Road intersection at parking location in Coniston near the gate to the dump road" 0 #FEATURES_copy0 -80.850659727547,46.47695934174871,0 "road junction with train tracks" 0 #FEATURES_copy0 -80.9047668799261,46.4807160206343,0 "road junction" 0 #FEATURES_copy0 -80.9021279443224,46.4847996031152,0 "rotated by folding to 76 to 120; fold axis 204 plunge 42; Sud breccia is foliated" 0 #FEATURES_copy0 -80.8859813518101,46.4679824088056,0 "sandstone 0 #FEATURES_copy0 -80.8937563387326,46.4750815797177,0 "sandstone 212/83 younging west; folded to 085/72" 0 #FEATURES_copy0 -80.85330707943081,46.47588281656941,0 "sandstone 100/54" 0 #FEATURES_copy0 -80.8942003880879,46.4744880180898,0 "sandstone 120/58 younging west" 0 #FEATURES_copy0 -80.85238949954341,46.4779965401408,0 "sandstone 120/74" 0 #FEATURES_copy0 -80.85045569581112,46.48010893143151,0 "sandstone 130/58" 0 #FEATURES_copy0 -80.8846670372297,46.4735878424393,0 "sandstone 146/84" 0 #FEATURES_copy0 -80.8842285213488,46.47152649144291,0 "sandstone 150/74" 0 #FEATURES_copy0 -80.8839256616421,46.4730651158456,0 "sandstone 204/78" 0 #FEATURES_copy0 -80.85186460585339,46.4793997974271,0 "sandstone 206/58" 0 #FEATURES_copy0 -80.85257008019821,46.4786627426763,0 "sandstone 208/74" 0 #FEATURES_copy0 -80.85245128925661,46.4744147818683,0 "sandstone 214/50 younging SE" 0 #FEATURES_copy0 -80.8925845684585,46.4681507936539,0 "sandstone 214/72 younging west ?" 0 #FEATURES_copy0 -80.8523942691515,46.4762326263571,0 "sandstone 220/67" 0 #FEATURES_copy0 -80.85187542436491,46.47541299259161,0 "sandstone 260/70" 0 #FEATURES_copy0 -80.89656980610479,46.4683344590158,0 "sandstone 40/32 younging east; shatter cones point up" 0 #FEATURES_copy0 -80.8905156337525,46.4671498756775,0 "sandstone 46/82" 0 #FEATURES_copy0 -80.8540115261104,46.4755057349356,0 "sandstone 70/50" 0 #FEATURES_copy0 -80.8883645449547,46.4681467526105,0 "sandstone 70/78; Sudbury breccia" 0 #FEATURES_copy0 -80.8946443393654,46.4671897517084,0 "sandstone 80/60 folded to 186/72 (plunging 098) returning to 87/76" 0 #FEATURES_copy0 -80.85423434630459,46.4749930422367,0 "sandstone to the west" 0 #FEATURES_copy0 -80.82987764695299,46.5075558494947,0 "sandstone", subed, 202" 0 #FEATURES_copy0 -80.81498977379729,46.50070207992841,0 "sandstone", subed, 220, 50, "some breccia" 0 #FEATURES_copy0 -80.81868882844731,46.4974411637706,0 "sandstone, subed, 165" 0 #FEATURES_copy0 -80.82330703871,46.49188666016681,0 "sandstone, subed, 188" 0 #FEATURES_copy0 -80.8212445783128,46.49697720926571,0 "sandstone, subed, 198, 50" 0 #FEATURES_copy0 -80.8170691536472,46.4985545302692,0 "sandstone, subed, 208, ,"Sudbury breccia; E-W foliation in brecciaparticularly when breccia is E-W trending; rocks potentially rotated by fa 0 #FEATURES_copy0 -80.8162267992514,46.50101905849611,0 "Shatter cones point downwards to North; Laurentian University road side outcrops" 0 #FEATURES_copy0 -80.97951178727941,46.46873937388131,0 "Shawanaga shear pod" 0 #FEATURES_copy0 -80.2675299667679,45.5399792816413,0 "slump balls" 0 #FEATURES_copy0 -80.8112361698345,46.49323531086349,0 "strained agmatites" 0 #FEATURES_copy0 -81.0489352696063,46.51300861738901,0 "strike change 162/64 to 070; folds plunge 45; cross cut by Sud breccia" 0 #FEATURES_copy0 -80.88622992055372,46.4737064024527,0 "Sud breccia McKim Sediments; E-W Trap dikes cross-cut breccia and quartz diorite; see INCO guidebook for this locality which is just west 0 #FEATURES_copy0 -81.0747274710829,46.47126368473991,0 "Sud breccia in cross-bedded sandstone; sandstone 65/55 0 #FEATURES_copy0 -80.89976220659329,46.46761733292671,0 "Sud Breccia" 0 #FEATURES_copy0 -80.88406176879209,46.4703113764356,0 "Sud breccia" 0 #FEATURES_copy0 -80.89525171069511,46.469683200011,0 "Sud breccia" 0 #FEATURES_copy0 -80.8941277801997,46.47162607899092,0 "Sud breccia" 0 #FEATURES_copy0 -80.89346050705701,46.4731463914986,0 "Sud breccia" 0 #FEATURES_copy0 -80.89576197780519,46.4753084149817,0 "Sud breccia" 0 #FEATURES_copy0 -80.8966588283741,46.4763531815715,0 "Sud Breccia; 513670,5148622 bedding turns from 190 to 220" 0 #FEATURES_copy0 -80.82005181584511,46.4911616197139,0 "Sudbury breccia cut by F2 foliation; Plane Table lake" 0 #FEATURES_copy0 -81.7364684028376,46.2315916134527,0 "Sudbury diabase crossing the Dryden anorthosite" 0 #FEATURES_copy0 -80.7006093300764,46.4472812407554,0 "Sudbury diabase in 'fat' migmatites, Burwash locality" 0 #FEATURES_copy0 -80.8013546014831,46.2397581266015,0 "total retrogression of flattened aluminsilicate porphyroblasts in the stream" 0 #FEATURES_copy0 -81.00662119292841,46.3986336761015,0 "trap dike cutting granite; foliation in the chilled margin material of the dike 0 #FEATURES_copy0 -81.0690487834638,46.48191377027311,0 "trap dike locality" 0 #FEATURES_copy0 -82.46081118121842,46.1996367144268,0 "trap dike trending 276 intruded post foliation; foliation also represented by pseudobedding; Sudbury breccia on top of the outcrop is pre-ea 0 #FEATURES_copy0 -82.104075621283,46.20800418837331,0 "two sets of shatter cones point both west and downwards" 0 #FEATURES_copy0 -80.87970487662162,46.4850572053028,0 "western limit of completely recrystallized 'Grenville' gneisses; folded amphibolites; linear fabric oriented 140/490; Davidson's mylonite zo 0 #FEATURES_copy0 -80.9646252009733,46.36672432044781,0 "X-bedded sandstone with blebs" 0 #FEATURES_copy0 -80.8632363821872,46.51626715240791,0 "x-bedded sandstone; vein of pegmatite" 0 #FEATURES_copy0 -80.8225684622297,46.4906075779291,0 Red Deer Lake, Sudbury diabase north side of road 0 #FEATURES_copy0 -80.732183745165,46.404485080116,0 Red Deer Lake, Sudbury diabase north side of road 0 #FEATURES_copy0 -80.732183745165,46.404485080116,0 S-fold in quartzite, strike 95/steep, younging south 0 #FEATURES_copy0 -80.8416813403872,46.5363082662525,0 Feature Labels (COMMENTS_L) 0 1 " (north of the rail tracks)" 0 #FEATURES_LABELS -80.8100887481142,46.48969658057041,0 " (this value is off by 1 km due to influence of the power line??) outcrop east side of the road at the power line" 0 #FEATURES_LABELS -80.85351717807311,46.5189369782109,0 "" 0 #FEATURES_LABELS -80.82137167574589,46.49398055326921,0 "(near railway), fine grained, rounded biotite-qtz-feldspar boulders, imbricated towards the west (Current?); E-W strike with relatively shal 0 #FEATURES_LABELS -80.8134134889854,46.5005105288303,0 "(west end of a small black outcrop); 15m wide cross cutting dike of Sudbury diabase striking 268" 0 #FEATURES_LABELS -80.8216340294854,46.4934499882882,0 "?" 0 #FEATURES_LABELS -80.88507125020691,46.467207531815,0 "20 degree contact between sandstone (west) and Nipissing gabbro (east)" 0 #FEATURES_LABELS -80.8371901506216,46.50744949742251,0 "agmatites with some bands of spotted (cordierite?) hornfels" 0 #FEATURES_LABELS -81.049003504765,46.51641041081041,0 "amphibolitized gabbro with patches of epidosite cut by pink granite that has suffered subsequent brittle deformation; 0 #FEATURES_LABELS -80.99964870018179,46.41069347135141,0 "Augen granite of the Creighton pluton" 0 #FEATURES_LABELS -81.0691068326876,46.4866025159102,0 "Balsam St intersection with highway 17; staurolite bearing meta-greywackes (turbidites); small shatter cones pointing 352 upwards" 0 #FEATURES_LABELS -82.101877106039,46.463766232952,0 "buff to pink weathering intermediate dike with small amphiolite needles; intrusion post-dates the regional shear deformation (foliation) see 0 #FEATURES_LABELS -81.0105283889289,46.4231935499536,0 "centre of bridge of highway" 0 #FEATURES_LABELS -80.8797051940189,46.4849132123792,0 "contact 030 between sandstone and Sud breccia" 0 #FEATURES_LABELS -80.885456908278,46.469628812343,0 "contact between Nipissing gabbro and 5 metre intermediate dike with amph. needles and garnet" 0 #FEATURES_LABELS -80.8218387181014,46.514563250988,0 "contact of fine grained Nipissing diabase and x-bedded sandstone" 0 #FEATURES_LABELS -80.8471675548427,46.50986614128,0 "contact of sandstone (with pyrrhotite) and Nipissing gabbro" 0 #FEATURES_LABELS -80.831767402976,46.50762164128721,0 "contact striking 110 between Nipissing gabbro and sandstone" 0 #FEATURES_LABELS -80.82474564604421,46.51458574076892,0 "contact with folded amphibolitic metagabbro" 0 #FEATURES_LABELS -82.09297378577541,46.2103518971402,0 "crenulation (148/90) wraps the staurolite in schists at the side of the road 0 #FEATURES_LABELS -81.0074145223154,46.3973556678727,0 "crossbedded" 0 #FEATURES_LABELS -80.81079794623101,46.4880868321566,0 "cut by Sud breccia' 0 #FEATURES_LABELS -80.82234561901632,46.51502301555,0 "deformed Sudbury breccia; granite sill in Mississagi Sandstones; highway to Long Lake" 0 #FEATURES_LABELS -81.01057987248871,46.42023265126619,0 "diabase either intruding or a clast in breccia; strike 120; dikelets cross cut Nipissing at 513642, 5148727" 0 #FEATURES_LABELS -80.8212482370638,46.4918834612623,0 "dike 010/64 of plag, amph-needles, garnet + Sud Breccia, shatter cones; bedding 184/74" 0 #FEATURES_LABELS -80.81883017300849,46.49019673717991,0 "downward pointing shatter cone locality near Anderson Lake 0 #FEATURES_LABELS -81.86492260291681,46.2207648989612,0 "drill site 267" 0 #FEATURES_LABELS -80.82535137672301,46.512687765452,0 "fold plunge 54/52 varying from 188/58 to 275/60" 0 #FEATURES_LABELS -80.8539428059911,46.47684658655621,0 "fold structure beds varying in orientation from 30/82 to 111/78; plunge 341" 0 #FEATURES_LABELS -80.8518495912147,46.475331962785,0 "folding Sud breccia" 0 #FEATURES_LABELS -80.85290247915719,46.47617028392621,0 "folding from 102/67 to 210/84 plunge east" 0 #FEATURES_LABELS -80.8533048061949,46.47672877537571,0 "folding from 217/85 (north limb) to 93/68 and back to 34/80" 0 #FEATURES_LABELS -80.8529812934995,46.475927396243,0 "foliated amphibolite likely Nipissing gabbro cutting distal greywackes now crenulated garnet-mica schist; foliated rocks and D2 folds are cu 0 #FEATURES_LABELS -82.46208263546382,46.1996834582921,0 "foliated Sudbury breccia" 0 #FEATURES_LABELS -80.88508595476981,46.47259830838681,0 "Garson Road, contact 343/50 between Sud breccia and sandstone" 0 #FEATURES_LABELS -80.8325523166309,46.51093462415831,0 "Garson Road, contact strike 164 of Nipissing and Sudbury breccia" 0 #FEATURES_LABELS -80.83355298569781,46.51192603379841,0 "Garson Road, contact strike 164 of Nipissing and Sudbury breccia" 0 #FEATURES_LABELS -80.8331119655315,46.5112144277395,0 "Garson Road, dike trending E-W" 0 #FEATURES_LABELS -80.83508390064981,46.51001134955801,0 "Garson Road, folds, with near horizontal axes, verging west" 0 #FEATURES_LABELS -80.8318123781572,46.5099435892511,0 "Garson_Coniston area" 0 #FEATURES_LABELS -80.819259658896,46.5100144388795,0 "Garson_Coniston area, Contact, strike 303, of Nipissing and sandstone; abundant cleaved Sudbury Breccia" . 0 #FEATURES_LABELS -80.80859607458932,46.5066222635592,0 "Garson_Coniston area, felsic dike with acicular amphibole 256/80" 0 #FEATURES_LABELS -80.80792916830261,46.4961366649549,0 "Garson_Coniston area, felsic dike with acicular amphibole 256/80" 0 #FEATURES_LABELS -80.80792916830261,46.4961366649549,0 "Garson_Coniston area, hill on the pipe line track on way out to the Garson Road" 0 #FEATURES_LABELS -80.82656840706081,46.50710090263991,0 "Garson_Coniston area, irregular felsic dike app. strike 244" 0 #FEATURES_LABELS -80.8063254122041,46.4963859484289,0 "Garson_Coniston area, lunch stop" 0 #FEATURES_LABELS -80.8063254122041,46.4963859484289,0 "Garson_Coniston area, view of anticline cut at the top by an E-W mafic trap dike strike 284; 0 #FEATURES_LABELS -80.8168348082483,46.5101275756952,0 "high strain zone in granite" 0 #FEATURES_LABELS -81.0490037879115,46.51672539416351,0 "highly (rutiliferous) 50 m wide altered Loon Lake fault zone (8786) separating the North and South deformation domains" 0 #FEATURES_LABELS -81.725926498845,46.20712496450721,0 "Hydro road junction with 17 east of Sudbury water works; travnum (col 4) 1 = wrc; 2 = krista; 3 = theresa; 4 = maria; 5 = grant 0 #FEATURES_LABELS -80.8154367445803,46.48800441559051,0 "isoclinally folded metasediments intruded by foliated granite; near small lake" 0 #FEATURES_LABELS -80.96891533266762,46.3897919170397,0 "Junction of Landing road and the Deer Lake Road" 0 #FEATURES_LABELS -80.73904992450829,46.4050949341801,0 "junction of road and side road on south side of the railway tracks" 0 #FEATURES_LABELS -80.88022658141961,46.4848057645946,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_LABELS -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_LABELS -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_LABELS -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_LABELS -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_LABELS -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_LABELS -80.7564508864801,46.4152399783552,0 "Junction of the Red Deer Lake road and highway 537 Wahnapitae to St Cloud (ophiolite dikes???)" 0 #FEATURES_LABELS -80.7564508864801,46.4152399783552,0 "location of bridge south of the pumping station" 0 #FEATURES_LABELS -80.8383803806521,46.5104570322177,0 "McKim turbidites; chloritoids wrapped in S2 foliation predate the main foliation" 0 #FEATURES_LABELS -81.77855709743029,46.2713716484479,0 "Murray Mine plaque; south along the rail track one encounters aphyric and plag-phyric mafic units pink granite, grey monzodiorite/granodio 0 #FEATURES_LABELS -81.05203248981169,46.5211878205103,0 "Nipissing gabbro" 0 #FEATURES_LABELS -80.88781530472291,46.46921716811571,0 "Nobel eclogite? Body" 0 #FEATURES_LABELS -80.10523404759761,45.4233110981542,0 "outcrop west of rail track before the bend approaching Coniston; Sudbury breccia but some beds possibly striking 280" 0 #FEATURES_LABELS -80.843312512071,46.49966443759261,0 "Outcrops of X-bedded sandstone at the western margin of the Nipissing diabase east of the Garson road to the south of the gravel quarry; Z-f 0 #FEATURES_LABELS -80.8391564417164,46.499244689306,0 "outcrops with large staurolite xls; on east side of the road are beautifully preserved soft sedimentary structures (sheath-like folds); thes 0 #FEATURES_LABELS -81.04913824926931,46.50680784843921,0 "pegmatite spiral in Nipissing" 0 #FEATURES_LABELS -80.8420472719109,46.5360387871656,0 "photograph of metasandstone with a shatter cone and blebs" 0 #FEATURES_LABELS -80.8637859731757,46.5154398514212,0 "Point zero at road side " 0 #FEATURES_LABELS -80.8433617701279,46.5324227950819,0 "Red Deer Lake agmatite, south side of road" 0 #FEATURES_LABELS -80.732196754651,46.4044851105813,0 "Red Deer Lake, Sudbury diabase north side of road" 0 #FEATURES_LABELS -80.732183745165,46.404485080116,0 "Red Deer Lake, Sudbury diabase outcrop north side of road" 0 #FEATURES_LABELS -80.732196754651,46.4044851105813,0 "Road intersection at parking location in Coniston near the gate to the dump road" 0 #FEATURES_LABELS -80.850659727547,46.47695934174871,0 "road junction with train tracks" 0 #FEATURES_LABELS -80.9047668799261,46.4807160206343,0 "road junction" 0 #FEATURES_LABELS -80.9021279443224,46.4847996031152,0 "rotated by folding to 76 to 120; fold axis 204 plunge 42; Sud breccia is foliated" 0 #FEATURES_LABELS -80.8859813518101,46.4679824088056,0 "sandstone 0 #FEATURES_LABELS -80.8937563387326,46.4750815797177,0 "sandstone 212/83 younging west; folded to 085/72" 0 #FEATURES_LABELS -80.85330707943081,46.47588281656941,0 "sandstone 100/54" 0 #FEATURES_LABELS -80.8942003880879,46.4744880180898,0 "sandstone 120/58 younging west" 0 #FEATURES_LABELS -80.85238949954341,46.4779965401408,0 "sandstone 120/74" 0 #FEATURES_LABELS -80.85045569581112,46.48010893143151,0 "sandstone 130/58" 0 #FEATURES_LABELS -80.8846670372297,46.4735878424393,0 "sandstone 146/84" 0 #FEATURES_LABELS -80.8842285213488,46.47152649144291,0 "sandstone 150/74" 0 #FEATURES_LABELS -80.8839256616421,46.4730651158456,0 "sandstone 204/78" 0 #FEATURES_LABELS -80.85186460585339,46.4793997974271,0 "sandstone 206/58" 0 #FEATURES_LABELS -80.85257008019821,46.4786627426763,0 "sandstone 208/74" 0 #FEATURES_LABELS -80.85245128925661,46.4744147818683,0 "sandstone 214/50 younging SE" 0 #FEATURES_LABELS -80.8925845684585,46.4681507936539,0 "sandstone 214/72 younging west ?" 0 #FEATURES_LABELS -80.8523942691515,46.4762326263571,0 "sandstone 220/67" 0 #FEATURES_LABELS -80.85187542436491,46.47541299259161,0 "sandstone 260/70" 0 #FEATURES_LABELS -80.89656980610479,46.4683344590158,0 "sandstone 40/32 younging east; shatter cones point up" 0 #FEATURES_LABELS -80.8905156337525,46.4671498756775,0 "sandstone 46/82" 0 #FEATURES_LABELS -80.8540115261104,46.4755057349356,0 "sandstone 70/50" 0 #FEATURES_LABELS -80.8883645449547,46.4681467526105,0 "sandstone 70/78; Sudbury breccia" 0 #FEATURES_LABELS -80.8946443393654,46.4671897517084,0 "sandstone 80/60 folded to 186/72 (plunging 098) returning to 87/76" 0 #FEATURES_LABELS -80.85423434630459,46.4749930422367,0 "sandstone to the west" 0 #FEATURES_LABELS -80.82987764695299,46.5075558494947,0 "sandstone", subed, 202" 0 #FEATURES_LABELS -80.81498977379729,46.50070207992841,0 "sandstone", subed, 220, 50, "some breccia" 0 #FEATURES_LABELS -80.81868882844731,46.4974411637706,0 "sandstone, subed, 165" 0 #FEATURES_LABELS -80.82330703871,46.49188666016681,0 "sandstone, subed, 188" 0 #FEATURES_LABELS -80.8212445783128,46.49697720926571,0 "sandstone, subed, 198, 50" 0 #FEATURES_LABELS -80.8170691536472,46.4985545302692,0 "sandstone, subed, 208, ,"Sudbury breccia; E-W foliation in brecciaparticularly when breccia is E-W trending; rocks potentially rotated by fa 0 #FEATURES_LABELS -80.8162267992514,46.50101905849611,0 "Shatter cones point downwards to North; Laurentian University road side outcrops" 0 #FEATURES_LABELS -80.97951178727941,46.46873937388131,0 "Shawanaga shear pod" 0 #FEATURES_LABELS -80.2675299667679,45.5399792816413,0 "slump balls" 0 #FEATURES_LABELS -80.8112361698345,46.49323531086349,0 "strained agmatites" 0 #FEATURES_LABELS -81.0489352696063,46.51300861738901,0 "strike change 162/64 to 070; folds plunge 45; cross cut by Sud breccia" 0 #FEATURES_LABELS -80.88622992055372,46.4737064024527,0 "Sud breccia McKim Sediments; E-W Trap dikes cross-cut breccia and quartz diorite; see INCO guidebook for this locality which is just west 0 #FEATURES_LABELS -81.0747274710829,46.47126368473991,0 "Sud breccia in cross-bedded sandstone; sandstone 65/55 0 #FEATURES_LABELS -80.89976220659329,46.46761733292671,0 "Sud Breccia" 0 #FEATURES_LABELS -80.88406176879209,46.4703113764356,0 "Sud breccia" 0 #FEATURES_LABELS -80.89525171069511,46.469683200011,0 "Sud breccia" 0 #FEATURES_LABELS -80.8941277801997,46.47162607899092,0 "Sud breccia" 0 #FEATURES_LABELS -80.89346050705701,46.4731463914986,0 "Sud breccia" 0 #FEATURES_LABELS -80.89576197780519,46.4753084149817,0 "Sud breccia" 0 #FEATURES_LABELS -80.8966588283741,46.4763531815715,0 "Sud Breccia; 513670,5148622 bedding turns from 190 to 220" 0 #FEATURES_LABELS -80.82005181584511,46.4911616197139,0 "Sudbury breccia cut by F2 foliation; Plane Table lake" 0 #FEATURES_LABELS -81.7364684028376,46.2315916134527,0 "Sudbury diabase crossing the Dryden anorthosite" 0 #FEATURES_LABELS -80.7006093300764,46.4472812407554,0 "Sudbury diabase in 'fat' migmatites, Burwash locality" 0 #FEATURES_LABELS -80.8013546014831,46.2397581266015,0 "total retrogression of flattened aluminsilicate porphyroblasts in the stream" 0 #FEATURES_LABELS -81.00662119292841,46.3986336761015,0 "trap dike cutting granite; foliation in the chilled margin material of the dike 0 #FEATURES_LABELS -81.0690487834638,46.48191377027311,0 "trap dike locality" 0 #FEATURES_LABELS -82.46081118121842,46.1996367144268,0 "trap dike trending 276 intruded post foliation; foliation also represented by pseudobedding; Sudbury breccia on top of the outcrop is pre-ea 0 #FEATURES_LABELS -82.104075621283,46.20800418837331,0 "two sets of shatter cones point both west and downwards" 0 #FEATURES_LABELS -80.87970487662162,46.4850572053028,0 "western limit of completely recrystallized 'Grenville' gneisses; folded amphibolites; linear fabric oriented 140/490; Davidson's mylonite zo 0 #FEATURES_LABELS -80.9646252009733,46.36672432044781,0 "X-bedded sandstone with blebs" 0 #FEATURES_LABELS -80.8632363821872,46.51626715240791,0 "x-bedded sandstone; vein of pegmatite" 0 #FEATURES_LABELS -80.8225684622297,46.4906075779291,0 Red Deer Lake, Sudbury diabase north side of road 0 #FEATURES_LABELS -80.732183745165,46.404485080116,0 Red Deer Lake, Sudbury diabase north side of road 0 #FEATURES_LABELS -80.732183745165,46.404485080116,0 S-fold in quartzite, strike 95/steep, younging south 0 #FEATURES_LABELS -80.8416813403872,46.5363082662525,0 2002 0 2003 0 00map1_03 Events 0 Exported from 00map1_03 Events on 2008-04-25 normal #sn_red-circle_copy1 highlight #sn_red-circle_copy2 Features 0 1 "2 metre dike of granite trending 140, 90. Granite is foliated" 0 #sn_red-circle_copy0 -81.06710096935331,46.4871166860031,0 "Agglomeratic breccia" 0 #sn_red-circle_copy0 -81.0546051060192,46.5124030824989,0 "axis of Coniston syncline south of hwy 17 west of Sudbury Water Treatment Plant" 0 #sn_red-circle_copy0 -80.8297720211558,46.4871086918282,0 "Ball and pillow locality on hwy 144 near the turn off to Clara Belle" 0 #sn_red-circle_copy0 -81.0483951747198,46.50665517300281,0 "Bend in road; large outcrop east side of road" 0 #sn_red-circle_copy0 -81.46472138068872,46.3865929559394,0 "breccia plus melt?; photo" 0 #sn_red-circle_copy0 -81.06136582309701,46.5082868665486,0 "clasts of foliated and porphyroblastic rocks in breccia" 0 #sn_red-circle -81.05020970657721,46.5097052353342,0 "contact of volcanics and seds, strike 040 90" 0 #sn_red-circle_copy0 -81.05364861089922,46.5074087912937,0 "Continuation of pillow lava - sed contact" 0 #sn_red-circle_copy0 -81.0673521712108,46.5006248837148,0 "East of Lady Macdonald Lake,i.e. east of Creighton granite; change in orientation fro 0 #sn_red-circle_copy0 -81.0666438555841,46.4862259953058,0 "Folded cleavage loclity nr Anderson Lake" 0 #sn_red-circle_copy0 -81.7369054881186,46.22936579422871,0 "Foliated pillow lavas" 0 #sn_red-circle_copy0 -81.0510287875251,46.5074549877458,0 "High point on Nipissing gabbro" 0 #sn_red-circle_copy0 -81.47979202868019,46.40113729134,0 "Junction of farm road with main road after the1st power line" 0 #sn_red-circle_copy0 -81.4659922942196,46.3892247094445,0 "Junction of hwy 17 with side road to Hydro Plant near Sudbury water treatment plant" 0 #sn_red-circle_copy0 -80.81543686633511,46.4879684174862,0 "Junction of Spanish River road with the Inco High Falls road" 0 #sn_red-circle_copy0 -81.4622711464008,46.3844339475221,0 "junction of two roads" 0 #sn_red-circle_copy0 -81.0577954944991,46.5093146738297,0 "Norite sublayer breccia" 0 #sn_red-circle_copy0 -81.46232716682091,46.43880095442971,0 "pillow lava contact with seds" 0 #sn_red-circle_copy0 -81.06848680375531,46.5012631782262,0 "Plane Table Lake" 0 #sn_red-circle_copy0 -81.7261268480155,46.100247155071,0 "Pylon line crossing road" 0 #sn_red-circle_copy0 -81.3330743501663,4.64737888489604,0 "S-shaped fold w an axial plane foliation and randomly oriented staurolite; photo" 0 #sn_red-circle_copy0 -81.06694404359629,46.4866488000605,0 "sed unit north of basalt unit strike 223 dip 80" 0 #sn_red-circle_copy0 -81.05580022277501,46.5083617133254,0 "Shatter cone locality nr Anderson Lake" 0 #sn_red-circle_copy0 -81.73529867874112,46.22169012452321,0 "Slump ball locality" 0 #sn_red-circle_copy0 -81.0483691307127,46.5066821826492,0 "Staurolitic seds, strike 172 90; cleavaage 90 90 0 #sn_red-circle_copy0 -81.0615808421129,46.5024730445228,0 "Trap dike locality" 0 #sn_red-circle_copy0 -81.0690617090394,46.48183276622391,0 "Two directions of shatter coning on the Sudbury - North Bay bypass" 0 #sn_red-circle_copy0 -80.8801339768544,46.48544463764951,0 "undeformed pillow lavas" 0 #sn_red-circle_copy0 -81.0512399472957,46.5102357512281,0 Murray Plaque 0 #sn_red-circle_copy0 -81.0533361116247,46.5210612268061,0 Feature Labels (COMMENT_LO) 0 1 "2 metre dike of granite trending 140, 90. Granite is foliated" 0 #FEATURES_LABELS0 -81.06710096935331,46.4871166860031,0 "Agglomeratic breccia" 0 #FEATURES_LABELS0 -81.0546051060192,46.5124030824989,0 "axis of Coniston syncline south of hwy 17 west of Sudbury Water Treatment Plant" 0 #FEATURES_LABELS0 -80.8297720211558,46.4871086918282,0 "Ball and pillow locality on hwy 144 near the turn off to Clara Belle" 0 #FEATURES_LABELS0 -81.0483951747198,46.50665517300281,0 "Bend in road; large outcrop east side of road" 0 #FEATURES_LABELS0 -81.46472138068872,46.3865929559394,0 "breccia plus melt?; photo" 0 #FEATURES_LABELS0 -81.06136582309701,46.5082868665486,0 "clasts of foliated and porphyroblastic rocks in breccia" 0 #sn_palette-4 -81.05020970657721,46.5097052353342,0 "contact of volcanics and seds, strike 040 90" 0 #FEATURES_LABELS0 -81.05364861089922,46.5074087912937,0 "Continuation of pillow lava - sed contact" 0 #FEATURES_LABELS0 -81.0673521712108,46.5006248837148,0 "East of Lady Macdonald Lake,i.e. east of Creighton granite; change in orientation fro 0 #FEATURES_LABELS0 -81.0666438555841,46.4862259953058,0 "Folded cleavage loclity nr Anderson Lake" 0 #FEATURES_LABELS0 -81.7369054881186,46.22936579422871,0 "Foliated pillow lavas" 0 #FEATURES_LABELS0 -81.0510287875251,46.5074549877458,0 "High point on Nipissing gabbro" 0 #FEATURES_LABELS0 -81.47979202868019,46.40113729134,0 "Junction of farm road with main road after the1st power line" 0 #FEATURES_LABELS0 -81.4659922942196,46.3892247094445,0 "Junction of hwy 17 with side road to Hydro Plant near Sudbury water treatment plant" 0 #FEATURES_LABELS0 -80.81543686633511,46.4879684174862,0 "Junction of Spanish River road with the Inco High Falls road" 0 #FEATURES_LABELS0 -81.4622711464008,46.3844339475221,0 "junction of two roads" 0 #FEATURES_LABELS0 -81.0577954944991,46.5093146738297,0 "Norite sublayer breccia" 0 #FEATURES_LABELS0 -81.46232716682091,46.43880095442971,0 "pillow lava contact with seds" 0 #FEATURES_LABELS0 -81.06848680375531,46.5012631782262,0 "Plane Table Lake" 0 #FEATURES_LABELS0 -81.7261268480155,46.100247155071,0 "Pylon line crossing road" 0 #FEATURES_LABELS0 -81.3330743501663,4.64737888489604,0 "S-shaped fold w an axial plane foliation and randomly oriented staurolite; photo" 0 #FEATURES_LABELS0 -81.06694404359629,46.4866488000605,0 "sed unit north of basalt unit strike 223 dip 80" 0 #FEATURES_LABELS0 -81.05580022277501,46.5083617133254,0 "Shatter cone locality nr Anderson Lake" 0 #FEATURES_LABELS0 -81.73529867874112,46.22169012452321,0 "Slump ball locality" 0 #FEATURES_LABELS0 -81.0483691307127,46.5066821826492,0 "Staurolitic seds, strike 172 90; cleavaage 90 90 0 #FEATURES_LABELS0 -81.0615808421129,46.5024730445228,0 "Trap dike locality" 0 #FEATURES_LABELS0 -81.0690617090394,46.48183276622391,0 "Two directions of shatter coning on the Sudbury - North Bay bypass" 0 #FEATURES_LABELS0 -80.8801339768544,46.48544463764951,0 "undeformed pillow lavas" 0 #FEATURES_LABELS0 -81.0512399472957,46.5102357512281,0 Murray Plaque 0 #FEATURES_LABELS0 -81.0533361116247,46.5210612268061,0 Worthington and west 0 Maps 0 Local 0 2360 (Great Bend) 0 2360_3_1.jpg 0.75 46.46115198837047 46.32369339471403 -81.40335400651732 -81.77633016836465 0.9171201289871713 Garson_rd_Nipp-gabbro contacts2x 0 #msn_ylw-pushpin_copy282121 1 -80.83743661842584,46.50797536724339,0 -80.83721255897117,46.50811440330774,0 -80.83702022745985,46.50824508609893,0 -80.83681098472124,46.508388292141,0 -80.83662667535619,46.50860042245809,0 -80.83653858292107,46.50877056425975,0 -80.83640356092852,46.50898419547746,0 -80.83636496550888,46.50916759792504,0 -80.83633942032424,46.50941486227957,0 -80.83631553338914,46.50970911142392,0 -80.83631901612247,46.50994427327175,0 -80.83631051967315,46.51015979637074,0 -80.83624629338161,46.51050410199955,0 -80.83612182132318,46.51071256118937,0 -80.83603659386534,46.5108233529372,0 Nipissing 0 -81.53745891856332 46.39166313193763 0 3471.160093246399 0 0.613342085116799 relativeToGround #msn_ylw-pushpin_copy140 -81.53917897190924,46.38766077392873,0 Nipissing 0 -81.53741037663602 46.39014625567702 0 3471.160093242862 0 0.6133772109065916 relativeToGround #msn_ylw-pushpin_copy3000 -81.54072881251149,46.3923211803276,0 Ramsay Lake_Pecors_Nipissing 0 -81.5111946583576 46.37869871412612 0 16532.62602974261 2.457673301287391e-012 0.6323521154126955 relativeToGround #msn_ylw-pushpin107 -81.53967287656283,46.39069403707938,0 2004 0 00map1_04 Events 0 Exported from 00map1_04 Events on 2008-04-25 normal #FEATURES_copy10 highlight #FEATURES_copy20 Features 0 "?" 0 #FEATURES_copy00 -81.0508787594307,46.5142947025827,0 "Amphibolite w. crse acic. Amph., south of very coarse mela-gabbro; bounded to south by seds" 0 #FEATURES_copy00 -81.0466253475107,46.50535007419751,0 "Ball and pillow locality on hwy 144, opp. Entrance to Clara Belle" 0 #FEATURES_copy00 -81.0482743099178,46.5066102263579,0 "Coarse Mafic gabbro contact with Stobie Qzte, north of ridge" 0 #FEATURES_copy00 -81.043128510461,46.510581079628,0 "Contact, Murray Gran. And Elsie Mnt pillows; linear fabric in granite w. acic. Amph." 0 #FEATURES_copy00 -81.0455602432519,46.5111309085645,0 "Coppercliffe offset dike at Bruce St" 0 #FEATURES_copy00 -81.0752728309579,46.4711553319358,0 "Garson photo traverse from Hwy 17, stp 1 " 0 #FEATURES_copy00 -80.8801211258891,46.48536362798021,0 "Garson photo traverse from Hwy 17, stp 2" 0 #FEATURES_copy00 -80.73505709923251,46.50151681497291,0 "Garson photo traverse from Hwy 17, stp 3" 0 #FEATURES_copy00 -80.7340977726173,46.497797770882,0 "Garson photo traverse from Hwy 17, stp 4" 0 #FEATURES_copy00 -80.73430337405659,46.495719349397,0 "Garson photo traverse from Hwy 17, stp 5" 0 #FEATURES_copy00 -80.73572748373989,46.4949576854697,0 "Garson photo traverse from Hwy 17, stp 6" 0 #FEATURES_copy00 -80.8105353881585,46.4886533707532,0 "hwy 144 to Clara Belle rail track, stp 1, volcanic breccia" 0 #FEATURES_copy00 -81.0546826564955,46.5133029988271,0 "hwy 144 to Clara Belle rail track, stp 2, graded volcanogenic breccia" 0 #FEATURES_copy00 -81.0545352055555,46.5127630972133,0 "hwy 144 to Clara Belle rail track, stp 3, folded Elsie Mntn. sediments " 0 #FEATURES_copy00 -81.055422312552,46.50921685337291,0 "hwy 144 to Clara Belle rail track, stp 4, ?" 0 #FEATURES_copy00 -81.05572143832499,46.5084337480579,0 "hwy 144 to Clara Belle rail track, stp 5 - pillow lavas strike 10" 0 #FEATURES_copy00 -81.06287360974322,46.50780907201381,0 "hwy 144 to Clara Belle rail track, stp 6, Rail trask, seds strike 10 vertical" 0 #FEATURES_copy00 -81.06399088285311,46.5055675660814,0 "hwy 144 to Clara Belle rail track, stp 7, shear juxtaposing staur. Metaseds. With volcanics; staur re-oriented into the shear orientation" 0 #FEATURES_copy00 -81.0604506419502,46.50437255218001,0 "Just north of Clara Belle mill area, south of lake and east of tracks, pillows cut by thick dikes, str. 120 (Ne end of outcrop" 0 #FEATURES_copy00 -81.05837428316841,46.5016917649701,0 "Just north of Clara Belle mill area, south of lake and east of tracks, Stobie seds., str. 40-60 vert, cut by gabbro" 0 #FEATURES_copy00 -81.0531056125258,46.501658334219,0 "Just north of Clara Belle mill area, south of lake and east of tracks, stp 2 Trap? Dike str 114, vert., visible contact on north side of dike, contains xenol. Of porph. Creighton granite w. angular phenocrysts of K-feldspar" 0 #FEATURES_copy00 -81.05863243825141,46.5015476401082,0 "Just north of Clara Belle mill area, south of lake and east of tracks, stp 2, repeat waypoint measurement" 0 #FEATURES_copy00 -81.05864143085191,46.5015476354983,0 "Long Lake staurolite locality" 0 #FEATURES_copy00 -81.0102885310143,46.42314857340631,0 "Long Lake staurolite locality" 0 #FEATURES_copy00 -81.00682047016271,46.39751769973249,0 "Murray Plaque" 0 #FEATURES_copy00 -81.0534811248306,46.5210989570856,0 "Nobel eclogite locality" 0 #FEATURES_copy00 -81.05354514356741,46.5215021056499,0 "Parry Sound Business exit off hwy 69 0 #FEATURES_copy00 -80.01849514707961,45.3626588412691,0 "Pillow lava ?" 0 #FEATURES_copy00 -81.0488502432403,46.5071499544338,0 "Pronto Mine parking area" 0 #FEATURES_copy00 -82.7204108166038,46.2086331410334,0 "Pronto Mine turn off hwy 17" 0 #FEATURES_copy00 -82.7188123847305,46.1977039624348,0 "Road sign 144/35 North to Timmins on La Salle; GPS test" 0 #FEATURES_copy00 -81.0292970154722,46.5066796579821,0 "Stobie Southeast of power station hway 144 Cara Belle, breccia at gabbro/quartzite contact" 0 #FEATURES_copy00 -81.0401021468811,46.50059268556209,0 "Stobie, Southeast of power station on hwy 144 nt jnct w. Clara Belle rd, Contact between foliated mafic, greenish metagabbro, and fresher looking, darker, gabbro to the north; latter has pegmatoid patches" 0 #FEATURES_copy00 -81.03863497514951,46.50321205986071,0 "Stobie, Southeast of power station on hwy 144 nt jnct w. Clara Belle rd, S-folds baked at contact w. diabase; very coarse staur. Schist w. some quartzite beds that seem to be boudinaged; Sudbury breccia contains blocks of foliated and porphyrobalstic sc 0 #FEATURES_copy00 -81.0394137269019,46.5057652356085,0 "Stobie, Southeast of power station on hwy 144 nt jnct w. Clara Belle rd, strongly foliated amphibolite" 0 #FEATURES_copy00 -81.0401589155482,46.50317553677991,0 "Stobie, Southeast of power station on hwy 144 nt jnct w. Clara Belle rd,Trap? Dike cutting schist" 0 #FEATURES_copy00 -81.03951842411659,46.5054552551518,0 Feature Labels (COMMENT_LO) 0 "?" 0 #FEATURES_LABELS1 -81.0508787594307,46.5142947025827,0 "Amphibolite w. crse acic. Amph., south of very coarse mela-gabbro; bounded to south by seds" 0 #FEATURES_LABELS1 -81.0466253475107,46.50535007419751,0 "Ball and pillow locality on hwy 144, opp. Entrance to Clara Belle" 0 #FEATURES_LABELS1 -81.0482743099178,46.5066102263579,0 "Coarse Mafic gabbro contact with Stobie Qzte, north of ridge" 0 #FEATURES_LABELS1 -81.043128510461,46.510581079628,0 "Contact, Murray Gran. And Elsie Mnt pillows; linear fabric in granite w. acic. Amph." 0 #FEATURES_LABELS1 -81.0455602432519,46.5111309085645,0 "Coppercliffe offset dike at Bruce St" 0 #FEATURES_LABELS1 -81.0752728309579,46.4711553319358,0 "Garson photo traverse from Hwy 17, stp 1 " 0 #FEATURES_LABELS1 -80.8801211258891,46.48536362798021,0 "Garson photo traverse from Hwy 17, stp 2" 0 #FEATURES_LABELS1 -80.73505709923251,46.50151681497291,0 "Garson photo traverse from Hwy 17, stp 3" 0 #FEATURES_LABELS1 -80.7340977726173,46.497797770882,0 "Garson photo traverse from Hwy 17, stp 4" 0 #FEATURES_LABELS1 -80.73430337405659,46.495719349397,0 "Garson photo traverse from Hwy 17, stp 5" 0 #FEATURES_LABELS1 -80.73572748373989,46.4949576854697,0 "Garson photo traverse from Hwy 17, stp 6" 0 #FEATURES_LABELS1 -80.8105353881585,46.4886533707532,0 "hwy 144 to Clara Belle rail track, stp 1, volcanic breccia" 0 #FEATURES_LABELS1 -81.0546826564955,46.5133029988271,0 "hwy 144 to Clara Belle rail track, stp 2, graded volcanogenic breccia" 0 #FEATURES_LABELS1 -81.0545352055555,46.5127630972133,0 "hwy 144 to Clara Belle rail track, stp 3, folded Elsie Mntn. sediments " 0 #FEATURES_LABELS1 -81.055422312552,46.50921685337291,0 "hwy 144 to Clara Belle rail track, stp 4, ?" 0 #FEATURES_LABELS1 -81.05572143832499,46.5084337480579,0 "hwy 144 to Clara Belle rail track, stp 5 - pillow lavas strike 10" 0 #FEATURES_LABELS1 -81.06287360974322,46.50780907201381,0 "hwy 144 to Clara Belle rail track, stp 6, Rail trask, seds strike 10 vertical" 0 #FEATURES_LABELS1 -81.06399088285311,46.5055675660814,0 "hwy 144 to Clara Belle rail track, stp 7, shear juxtaposing staur. Metaseds. With volcanics; staur re-oriented into the shear orientation" 0 #FEATURES_LABELS1 -81.0604506419502,46.50437255218001,0 "Just north of Clara Belle mill area, south of lake and east of tracks, pillows cut by thick dikes, str. 120 (Ne end of outcrop" 0 #FEATURES_LABELS1 -81.05837428316841,46.5016917649701,0 "Just north of Clara Belle mill area, south of lake and east of tracks, Stobie seds., str. 40-60 vert, cut by gabbro" 0 #FEATURES_LABELS1 -81.0531056125258,46.501658334219,0 "Just north of Clara Belle mill area, south of lake and east of tracks, stp 2 Trap? Dike str 114, vert., visible contact on north side of dike, contains xenol. Of porph. Creighton granite w. angular phenocrysts of K-feldspar" 0 #FEATURES_LABELS1 -81.05863243825141,46.5015476401082,0 "Just north of Clara Belle mill area, south of lake and east of tracks, stp 2, repeat waypoint measurement" 0 #FEATURES_LABELS1 -81.05864143085191,46.5015476354983,0 "Long Lake staurolite locality" 0 #FEATURES_LABELS1 -81.0102885310143,46.42314857340631,0 "Long Lake staurolite locality" 0 #FEATURES_LABELS1 -81.00682047016271,46.39751769973249,0 "Murray Plaque" 0 #FEATURES_LABELS1 -81.0534811248306,46.5210989570856,0 "Nobel eclogite locality" 0 #FEATURES_LABELS1 -81.05354514356741,46.5215021056499,0 "Parry Sound Business exit off hwy 69 0 #FEATURES_LABELS1 -80.01849514707961,45.3626588412691,0 "Pillow lava ?" 0 #FEATURES_LABELS1 -81.0488502432403,46.5071499544338,0 "Pronto Mine parking area" 0 #FEATURES_LABELS1 -82.7204108166038,46.2086331410334,0 "Pronto Mine turn off hwy 17" 0 #FEATURES_LABELS1 -82.7188123847305,46.1977039624348,0 "Road sign 144/35 North to Timmins on La Salle; GPS test" 0 #FEATURES_LABELS1 -81.0292970154722,46.5066796579821,0 "Stobie Southeast of power station hway 144 Cara Belle, breccia at gabbro/quartzite contact" 0 #FEATURES_LABELS1 -81.0401021468811,46.50059268556209,0 "Stobie, Southeast of power station on hwy 144 nt jnct w. Clara Belle rd, Contact between foliated mafic, greenish metagabbro, and fresher looking, darker, gabbro to the north; latter has pegmatoid patches" 0 #FEATURES_LABELS1 -81.03863497514951,46.50321205986071,0 "Stobie, Southeast of power station on hwy 144 nt jnct w. Clara Belle rd, S-folds baked at contact w. diabase; very coarse staur. Schist w. some quartzite beds that seem to be boudinaged; Sudbury breccia contains blocks of foliated and porphyrobalstic sc 0 #FEATURES_LABELS1 -81.0394137269019,46.5057652356085,0 "Stobie, Southeast of power station on hwy 144 nt jnct w. Clara Belle rd, strongly foliated amphibolite" 0 #FEATURES_LABELS1 -81.0401589155482,46.50317553677991,0 "Stobie, Southeast of power station on hwy 144 nt jnct w. Clara Belle rd,Trap? Dike cutting schist" 0 #FEATURES_LABELS1 -81.03951842411659,46.5054552551518,0 2005 0 05wrcmast Events 0 Exported from 05wrcmast Events on 2008-04-25 normal #FEATURES_copy11 highlight #FEATURES_copy21 Features 0 " 'frothy' volcanic facies recessive fragments in matrix with rounded?quartz xtals" 0 #FEATURES_copy01 -81.05423224812419,46.5044926635999,0 "cascade folding in metasedimentary unit east of the volcanic breccias" 0 #FEATURES_copy01 -81.05424065341229,46.5129432279406,0 "Creighton granite contact with offset diorite" 0 #FEATURES_copy01 -81.0690416640054,46.48658455611471,0 "east contact of diorite with rhyolite" 0 #FEATURES_copy01 -81.07569012443069,46.4703720913089,0 "eastern contact of McKim turb. and Coppercliff rhyolite" 0 #FEATURES_copy01 -81.0757681389002,46.47027304404271,0 "eastern contact of the diorite" 0 #FEATURES_copy01 -81.0770700574431,46.4698401933102,0 "eastern contact of trap dike in diorite" 0 #FEATURES_copy01 -81.07541726423349,46.47085824998901,0 "eastern contact of trap dike in diorite" 0 #FEATURES_copy01 -81.0750264273512,46.47080450942681,0 "gossan trench in diorite" 0 #FEATURES_copy01 -81.076600797475,46.46958851968741,0 "large pillow lava in road cut photo 0 #FEATURES_copy01 -81.0545169452264,46.51548996403411,0 "Matachewan dike with large phenos; photo" 0 #FEATURES_copy01 -81.05615126148069,46.5074975855526,0 "McKim graded turbidites w. erosional surface, flames, and rupups" 0 #FEATURES_copy01 -81.0740634625559,46.4714801070252,0 "mica schist fragments in diorite" 0 #FEATURES_copy01 -81.07704395629122,46.469804212487,0 "seemingly McKim sed" 0 #FEATURES_copy01 -81.07690043859451,46.4696333166298,0 "southern contact of diorite" 0 #FEATURES_copy01 -81.07695265326321,46.4697142779315,0 "Stobie contact with granite, contact strikes 137 steep to east" 0 #FEATURES_copy01 -81.0672821035942,46.48608162843251,0 "Stobie contact with granite, foliation strike 137 steep to east" 0 #FEATURES_copy01 -81.0672821035942,46.48608162843251,0 "Sudbury diabase chilled against gneiss (cairn), but also foliated" 0 #FEATURES_copy01 -80.8579864704631,46.4597704278026,0 "thin veins of Sudbury breccia with strong foliation strike 94 steep normal to the foliation strike 180 st 0 #FEATURES_copy01 -81.06805053745811,46.48585618442571,0 "thin veins of Sudbury breccia with strong foliation strike 94 steep normal to the foliation strike 180 st 0 #FEATURES_copy01 -81.06805053745811,46.48585618442571,0 "Trap dike 2 in Mississagi near the Grenville front" 0 #FEATURES_copy01 -80.8596517902924,46.4654602396593,0 "Trap dike cutting Elsie Mountain" 0 #FEATURES_copy01 -81.0555918928364,46.5085778037411,0 "Trap dike1 in Mississagi near the Grenville front" 0 #FEATURES_copy01 -80.8600511787253,46.46716165503931,0 "western contact of trap dike in diorite" 0 #FEATURES_copy01 -81.0757035365436,46.47065107005921,0 "worms of diorite? In sudbury breccia" 0 #FEATURES_copy01 -81.0766276812693,46.4701824754023,0 Azilda Grey Onaping 0 #FEATURES_copy01 -81.10933136791741,46.5598002183752,0 Chelmsford 0 #sn_pink-circle -81.1822260983254,46.56842779871352,0 Graded sstne, w. dewat. cracks, and concretions 0 #sn_pink-circle_copy0 -81.28744957703653,46.57377969871871,0 Onwatin slates 0 #sn_pink-circle_copy1 -81.32480961398503,46.58633467820476,0 Black Onaping 0 #sn_pink-circle_copy2 -81.383414265547,46.5909419775539,0 Grey Onaping 0 #sn_pink-circle_copy3 -81.3826337354423,46.5968932049549,0 Granophyre 0 #sn_pink-circle_copy4 -81.41182062729187,46.6174141093713,0 Craig Mine access road 0 #sn_pink-circle_copy5 -81.39496692882609,46.6322188721129,0 Craig Mine breccia outcrops 0 #FEATURES_copy01 -81.3445499679097,46.6750295874024,0 Craig Mine drill site 0 #FEATURES_copy01 -81.3315176934381,46.6584013863138,0 Craig Mine offices 0 #sn_pink-circle_copy6 -81.3690964437025,46.6374618836923,0 Craig Mine stripped line with breccias 0 #FEATURES_copy01 -81.3304177954235,46.6838185682923,0 Quartzite N. side of road; starting point for the student long traverse 0 #FEATURES_copy01 -80.81061590839171,46.4879785359915,0 Feature Labels (COMMENT_LO) 0 " 'frothy' volcanic facies recessive fragments in matrix with rounded?quartz xtals" 0 #FEATURES_LABELS2 -81.05423224812419,46.5044926635999,0 "cascade folding in metasedimentary unit east of the volcanic breccias" 0 #FEATURES_LABELS2 -81.05424065341229,46.5129432279406,0 "Creighton granite contact with offset diorite" 0 #FEATURES_LABELS2 -81.0690416640054,46.48658455611471,0 "east contact of diorite with rhyolite" 0 #FEATURES_LABELS2 -81.07569012443069,46.4703720913089,0 "eastern contact of McKim turb. and Coppercliff rhyolite" 0 #FEATURES_LABELS2 -81.0757681389002,46.47027304404271,0 "eastern contact of the diorite" 0 #FEATURES_LABELS2 -81.0770700574431,46.4698401933102,0 "eastern contact of trap dike in diorite" 0 #FEATURES_LABELS2 -81.07541726423349,46.47085824998901,0 "eastern contact of trap dike in diorite" 0 #FEATURES_LABELS2 -81.0750264273512,46.47080450942681,0 "gossan trench in diorite" 0 #FEATURES_LABELS2 -81.076600797475,46.46958851968741,0 "large pillow lava in road cut photo 0 #FEATURES_LABELS2 -81.0545169452264,46.51548996403411,0 "Matachewan dike with large phenos; photo" 0 #FEATURES_LABELS2 -81.05615126148069,46.5074975855526,0 "McKim graded turbidites w. erosional surface, flames, and rupups" 0 #FEATURES_LABELS2 -81.0740634625559,46.4714801070252,0 "mica schist fragments in diorite" 0 #FEATURES_LABELS2 -81.07704395629122,46.469804212487,0 "seemingly McKim sed" 0 #FEATURES_LABELS2 -81.07690043859451,46.4696333166298,0 "southern contact of diorite" 0 #FEATURES_LABELS2 -81.07695265326321,46.4697142779315,0 "Stobie contact with granite, contact strikes 137 steep to east" 0 #FEATURES_LABELS2 -81.0672821035942,46.48608162843251,0 "Stobie contact with granite, foliation strike 137 steep to east" 0 #FEATURES_LABELS2 -81.0672821035942,46.48608162843251,0 "Sudbury diabase chilled against gneiss (cairn), but also foliated" 0 #FEATURES_LABELS2 -80.8579864704631,46.4597704278026,0 "thin veins of Sudbury breccia with strong foliation strike 94 steep normal to the foliation strike 180 st 0 #FEATURES_LABELS2 -81.06805053745811,46.48585618442571,0 "thin veins of Sudbury breccia with strong foliation strike 94 steep normal to the foliation strike 180 st 0 #FEATURES_LABELS2 -81.06805053745811,46.48585618442571,0 "Trap dike 2 in Mississagi near the Grenville front" 0 #FEATURES_LABELS2 -80.8596517902924,46.4654602396593,0 "Trap dike cutting Elsie Mountain" 0 #FEATURES_LABELS2 -81.0555918928364,46.5085778037411,0 "Trap dike1 in Mississagi near the Grenville front" 0 #FEATURES_LABELS2 -80.8600511787253,46.46716165503931,0 "western contact of trap dike in diorite" 0 #FEATURES_LABELS2 -81.0757035365436,46.47065107005921,0 "worms of diorite? In sudbury breccia" 0 #FEATURES_LABELS2 -81.0766276812693,46.4701824754023,0 Azilda Grey Onaping 0 #FEATURES_LABELS2 -81.10933136791741,46.5598002183752,0 Craig Mine 0 #FEATURES_LABELS2 -81.1166680243274,46.5557702111387,0 Craig Mine 0 #FEATURES_LABELS2 -81.1822260983254,46.56842779871352,0 Craig Mine 0 #FEATURES_LABELS2 -81.2883923566676,46.57361809057601,0 Craig Mine 0 #FEATURES_LABELS2 -81.3258694642691,46.58626067519911,0 Craig Mine 0 #FEATURES_LABELS2 -81.383414265547,46.5909419775539,0 Craig Mine 0 #FEATURES_LABELS2 -81.3826337354423,46.5968932049549,0 Craig Mine 0 #FEATURES_LABELS2 -81.41133550575979,46.6148734021241,0 Craig Mine 0 #FEATURES_LABELS2 -81.39496692882609,46.6322188721129,0 Craig Mine breccia outcrops 0 #FEATURES_LABELS2 -81.3445499679097,46.6750295874024,0 Craig Mine drill site 0 #FEATURES_LABELS2 -81.3315176934381,46.6584013863138,0 Craig Mine offices 0 #FEATURES_LABELS2 -81.3690964437025,46.6374618836923,0 Craig Mine stripped line with breccias 0 #FEATURES_LABELS2 -81.3304177954235,46.6838185682923,0 Quartzite N. side of road; starting point for the student long traverse 0 #FEATURES_LABELS2 -80.81061590839171,46.4879785359915,0 Garson Rd 0 Gabbro-sed contact, Garson Rd 0 -80.83655334649703 46.50927524766514 0 284.0670273680601 0 -0.003844402289887788 relativeToGround #msn_ylw-pushpin_copy:0_copy10010 -80.83627279078323,46.50950640679731,0 G75 7, unit 21a Grenville qtz-diabase 0 -80.83972871708399 46.49483957989911 0 711.5612456373466 3.454971014465063e-013 0.08538926218906964 relativeToGround #sn_ylw-pushpin_copy:0_copy38003 -80.84022551577564,46.49640820417676,0 Grenville Front 0 Rock Unit Boundaries 0 1 Models 0 Bethune, 1997 0 Map http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune97fig3.jpg Textural evidence http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune97fig14.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune97fig15.jpg 0.75 46.1 45.9168 -81.0917 -81.3053 Haggart et al. 1993 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Haggartmodel.jpg 0.75 46.09930117261189 45.91614939216118 -80.93280848991259 -81.08986360939679 Maps - General 0 Card - Manitoulin 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Manitoulin_Card.jpg 0.75 46.50963912738729 46.17417569788994 -80.98627218469287 -81.33236219930411 Easton et al., 1999, Fig 9, Grenville Front Coniston_Wanapitei 0 c7ffffff http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/eastonfig8.jpg 0.75 46.53897079619361 46.42892276796068 -80.65655721550095 -80.8772434358437 Alice Lake 0 1st mylonite 0 -80.85952491159367 46.46049882159511 0 190.7679288598435 17.71473364112482 157.4777095964704 relativeToGround #msn_ylw-pushpin_copy:0_copy9500000010 -80.85931481157095,46.46049380061383,0 Maps 0 1 LaTour, T.E., 1968 0 9effffff http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/LaTour.jpg 0.75 46.46546264642532 46.45905771582358 -80.8528916575541 -80.86300845629046 -29.76152477995506 Alice Lake 0 -80.85832086079694 46.46425125080009 0 714.2439058088214 0 -0.0004459078310477621 relativeToGround #msn_ylw-pushpin_copy1190000001 -80.85518811348815,46.46389157985796,0 Trap dike - 510744, 5145964 0 -80.85994875330228 46.46724303593948 0 79.82069362705602 0 -0.002652027949532593 relativeToGround #msn_ylw-pushpin_copy015013 -80.86005332934781,46.46716421437773,0 Trap dike - 510776, 5145775 0 -80.85948334739435 46.46563641081715 0 79.82069362776333 3.366231317667411e-010 -0.002314621110946075 relativeToGround #msn_ylw-pushpin_copy31212020 -80.85964247755145,46.46545841283547,0 Trap dike cutting highly deformed 1.4? granite 0 -80.85802250474232 46.46484910212327 0 131.1410121871548 0 -0.0002296109760572509 relativeToGround #msn_ylw-pushpin0420102 -80.85795029264688,46.46476420230683,0 Pecors 0 -80.85821833743263 46.46351755796486 0 217.6250241507467 17.71480713169218 178.6684270795228 relativeToGround #msn_ylw-pushpin_copy:0_copy94010000 -80.85831928896755,46.46341163274763,0 Ramsay Lake conglom - Alice Lake 0 -80.8583581568486 46.46192727336219 0 202.8577724940999 17.71476672439982 -7.728567600286756 relativeToGround #msn_ylw-pushpin_copy:0_copy9201 -80.85905543613167,46.46220023690836,0 GF85 2b 0 Sud diab contact with gneiss - 510905,5145143 0 Outcrop http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/alicesuddiabcntct1a.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/alicesuddiabcntct1.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/alicesuddiabcntct2a.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/alicesuddiabcbtct3a.jpg Thin-sections http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/TS/GF852b-1.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/TS/GF852b-2.jpg Unmetamorphosed Sudbury Diabase, chilled margin, Whitefish Falls, Ontario http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/SuddiabwhiteFFallsTS.jpg -80.85844782733115 46.45948425882364 0 461.435459549471 0 157.4784904210281 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy1510 -80.85763649667075,46.45973926774381,0 GF85 3b - 2nd mylonite (cascade fold zone) 0 Outcrop Cascade folds - http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/myl2cascadem.jpg Thin-sections http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/TS/GF853b-1.jpg -80.85613103054084 46.45955294311182 0 513.1082687655691 0 0.001676312184904029 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy161111 -80.85615708939943,46.45946320104279,0 G75 29 Sudbury diabase, St Cloud rd west off 537 0 -80.81098672261882 46.43659157646079 0 948.3033938323766 2.146046752947455e-011 0.2347457825708906 relativeToGround #msn_ylw-pushpin_copy:0_copy5200111 -80.81116029917872,46.43463863982546,0 GF75 30Sudbury diabase (TS G1-41, 42); W end of St Cloud Rd 0 -80.83005905675299 46.43548001423796 0 1048.452595917722 6.263240001243635e-011 0.02033433650436511 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy170 -80.82703498319712,46.43500615574856,0 Brodil 0 K72 6 a-c, hwy 637 SW of Tyson Lake 0 -81.1448624715555 46.08785754441346 0 90.7346831749809 4.431055056392283e-010 -0.2064658509279962 relativeToGround #msn_ylw-pushpin_copy:0_copy28000130 -81.14510719304404,46.08786583276877,0 Maps 0 1 Henderson 0 Davidson 0 1 Davidson -stratigraphy 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Davidson/Brodil/davidsonmaps/davidsed1.gif 0.75 46.42467491848571 46.34524432024885 -80.9198952435592 -81.06599546219843 Davidson - structure 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Davidson/Brodil/davidsonmaps/davidstruc1.gif 0.75 46.42773342039027 46.3449190228249 -80.8964393634009 -81.06707087212951 -0.5266048102436328 Brodil Lake 0 -80.95103038958293 46.38092603527531 0 12310.76723121095 0 10.75224704263615 #msn_ylw-pushpin12112 -80.94204830479416,46.37293732431663,0 Bell Lake 0 Maps (Pryer) 0 Brooks sketch 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Brooks76fig1.jpg 0.75 46.10301825103798 46.10250884685977 -81.23292339887468 -81.23385554445274 0.5140350743758408 Pryer 1993, Fig 3. 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Pryer/pryerfig3.jpg 0.75 46.13816522760739 46.04552681319106 -81.15614411492744 -81.31420375198914 -0.1189782668036256 Pryer, 1993, Fig 1 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Pryer/pryerfig1.jpg 0.75 46.14712539016215 46.04288355935873 -81.08479173211565 -81.32023112264892 Bell Lake 0 -81.20654926026278 46.12867460785215 0 4277.774059608094 1.077042426354336e-024 0.006812834178399871 relativeToGround #msn_ylw-pushpin_copy2940500 -81.19871707696862,46.13345727470377,0 Balsam Lake 0 -81.2059836473107 46.15509123170072 0 4333.327215147413 0 0.007226111323551302 relativeToGround #msn_ylw-pushpin_copy1120010 -81.22283841928568,46.15733016730771,0 BeL68_24_1, Lorrain quartzite in contact with Bell Lake Granite; both units are foliated 0 -81.21366745229739 46.12235480590888 0 189.5341511464297 1.243305261601959e-011 0.001687955571424325 relativeToGround #msn_ylw-pushpin_copy900020 -81.21389991790009,46.12231638814059,0 BeL68_24_2, sheared non-porphyritic granite 0 -81.21108634675107 46.12562812578542 0 2657.051375946329 8.868808842618015e-013 0.003548526586631027 relativeToGround #msn_ylw-pushpin_copy530012 -81.21043485823709,46.12237889058685,0 BeL68_24_3, contact of porphyritic granite with Gowganda or Lorrain arkose 0 -81.18944211444494 46.1360436923481 0 301.6564924586502 7.498847845120529e-011 0.01915216144832408 relativeToGround #msn_ylw-pushpin_copy10012011 -81.18865062284914,46.13624668784882,0 BeL68_24_4, Goganda pelite 0 -81.19088738075419 46.13984502654788 0 1666.066305956716 1.357995230047409e-011 0.01811025983734736 relativeToGround #msn_ylw-pushpin_copy8220031 -81.19151641192109,46.13965994800696,0 BeL68_24_5, andalusite? bearing 2nd Gowganda pelite 0 -81.18785723481982 46.14469733728004 0 880.505442301436 2.569274573242275e-011 0.0202959258163918 relativeToGround #msn_ylw-pushpin_copy31133012 -81.19038434391204,46.14326419836705,0 BeL68_24_6, garnetiferous Gowganda pelite 0 -81.18785723481982 46.14469733728004 0 880.505442301436 2.569274573242275e-011 0.0202959258163918 relativeToGround #msn_ylw-pushpin_copy703102 -81.18737607088998,46.14305620460982,0 BeL68_24_7, garnet-biotite schist, north end of North Arm 0 -81.19935381559203 46.16107248383975 0 268.8435988736067 0 0.01200770420610515 relativeToGround #msn_ylw-pushpin_copy622000000 -81.19990202988421,46.16121848114544,0 BeL68_24_8, muscovite - chlorite schist, Gowganda pelite, south shore of Balsam Lake 0 -81.2059836473107 46.15509123170072 0 4333.327215147413 0 0.007226111323551302 relativeToGround #msn_ylw-pushpin_copy4120 -81.21064688342845,46.15772690473067,0 Deformed Sudbury diabase, Brooks, 1967 0 -81.23272965478495 46.10288413054212 0 546.9766520506049 1.10037329679408e-011 -0.01204572552416264 relativeToGround #msn_ylw-pushpin_copy00040012 -81.23301850128556,46.10275174400941,0 Broker_Atlee Lake 0 Broker Lake 0 -80.99245005492479 46.14653107335907 0 1276.385083165661 0 -0.0249770365875064 relativeToGround #msn_ylw-pushpin_copy:0_copy2411130 -80.99485213166194,46.14572028828573,0 Attlee Lake 0 -80.97448534998013 46.13927584092616 0 2733.270802943507 0 -0.01206764711768193 relativeToGround #msn_ylw-pushpin_copy:0_copy250000 -80.97856288673188,46.14040797995147,0 Maps 0 Bethune, K, 1989, Fig.3 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune89fig3b.jpg 0.75 46.15193473816778 46.14786974842191 -80.98719481603314 -80.99458570682131 3.170262185339037 Bethune, 1989, Fig 3a 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune89fig3a.jpg 0.75 46.15683119141992 46.12720681438768 -80.95167759635989 -81.02367208722524 0.2276177616379674 G75 3 Sudbury diabase (TS G1-24 6735); G72 3(TS G1-21 2378) 0 -80.99245072481675 46.14196401446237 0 3974.657151546512 6.670522522430225e-011 -13.46258290744492 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy50120 -80.9969142879531,46.13590495825633,0 Sud diab G75 2a (TS G1-23), SW contact visible; st 290 0 -81.00354412948171 46.13505683450326 0 322.178997312889 1.228264123242442e-010 -13.47058103797778 relativeToGround #msn_ylw-pushpin_copy1611010 -81.00403207447164,46.13502133515736,0 Sud diab G752b sheared dikelet in gneiss 0 -81.00354412948171 46.13505683450326 0 322.178997312889 1.228264123242442e-010 -13.47058103797778 relativeToGround #msn_ylw-pushpin_copy:0_copy980000000 -81.00369076129667,46.13506499171954,0 Mafic veinlets in gneiss 0 Outcrop http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/GrenmafveinKillrd.jpg Amphibolite veinlets in psephitic gneiss, west of diabase outcrop G75 23 -80.95973815025347 46.1541305522672 0 419.4371656600446 4.835929451724868e-011 0.002543921147226984 relativeToGround #msn_ylw-pushpin_copy:0_copy:002 -80.95988070160458,46.15399067160608,0 G75 26, deformed pegmatite in country rock gneiss, east side of G75 1; rock has a linear fabric 0 -80.98330392484277 46.14179396709303 0 86.69921184743856 0 -0.01693790376291676 relativeToGround #msn_ylw-pushpin_copy:0_copy7410010 -80.98333990835485,46.14174690239879,0 Schistose Sud diab G75 1; G72 2a (TSG1-19 2376, missing); highly strained Sud diab dikelet G72 2b (TS G1-20 2377) 0 Outcrop - schistose Sudbury diabase transected by narrow garnet-bearing mylonitized diabase http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/G752b%20Killarney%20rd.jpg -80.98330392484277 46.14179396709303 0 86.69921184743856 0 -0.01693790376291676 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy131120 -80.98347736640319,46.14172306196772,0 Sud Diabase G75 23 a,b,c; (TS G1-33) st 342;lat 503208, long 5111030; lat 46.1545, long -80.9581 0 1st metadiabase locality on the Killarney Road as shown on the Burwash sheet; NNW of Gainey Lake; relict cloudy zoned plag still present, but plag. is largely polygonized; relict plag now also has a crude pref. orient.; some plag. laths are well folded (see circle); polygonization seems to post date the deformation of the laths; garnet is intergrown with biotite in granular aggregates forming coronas to ore minerals; also present as symplectite coronas around plag. and as granular patches replacing plag. -80.95973815025347 46.1541305522672 0 419.4371656600446 4.835929451724868e-011 0.002543921147226984 relativeToGround #msn_ylw-pushpin_copy:0_copy97000002 -80.95930259954743,46.15417716636992,0 Fragmental rock 0 Outcrop http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/GrenfragrckKillrd.jpg -80.95973815025347 46.1541305522672 0 419.4371656600446 4.835929451724868e-011 0.002543921147226984 relativeToGround #msn_ylw-pushpin_copy:0_copy990040 -80.95970647958774,46.1540455231819,0 Sud diab G75 24 (TS G1-36 6750) 0 -81.00005103565313 46.13728767497997 0 1846.076076470695 1.026360852077988e-009 -0.3096052733523473 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy900 -81.00028109127227,46.13551218300268,0 Gneiss G75 25 a,b,c, 0 -81.00515203293099 46.13461252407323 0 322.1789973114744 9.168665808567179e-010 -0.3132828244348813 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy80000200 -81.00525495323254,46.13455524858116,0 Highway 69 0 Maps 0 Davidson, 200, fig8 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Davidson/Brodil/davidsonmaps/David01fig8.jpg 0.75 46.44245925105598 46.41214389711734 -80.86369476328072 -80.90584779106989 0.4674977405485176 Davidson, A., 1992 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Davidson/Killarney_Tyson/Davidson,%20A.,%201992,%20fig2Hwy69.jpg 0.75 46.47326094620655 46.42683594419894 -80.8419119782041 -80.93920918365366 Lumbers 1974, Burwash 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Lumbers,%20Burwash.jpg 0.75 46.50857082216107 46.34372773086749 -80.68642476605682 -81.01365319016621 Ames 2006 Alice Lake to Chief Lake 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Ames%20GF06-1.jpg 0.75 46.46686744220426 46.36800671284286 -80.85179784367409 -81.06716367776282 G66 1-14, mylonitized granite 0 -80.89719110833893 46.43002411028969 0 204.7441073499592 0 0.04365086098394781 #msn_ylw-pushpin20200002 -80.89719110833893,46.43002411028969,0 CBK69 10? 0 -80.89240417458575 46.42801301304949 0 1059.169154437511 2.652619766354094e-011 0.0471193115947158 relativeToGround #msn_ylw-pushpin_copy0210012 -80.89087872813624,46.42639831197362,0 CBK69 1-10 0 -80.89437085068643 46.42719952013795 0 1016.458654507908 4.152608758209849e-011 0.002298552419829365 relativeToGround #msn_ylw-pushpin_copy:0_copy36000002 -80.89604877310512,46.42850901086124,0 11.69.1 0 -80.89012772698098 46.42670743048837 0 1016.458654509322 6.146447532468089e-011 0.005372703704970313 relativeToGround #msn_ylw-pushpin_copy:0_copy39170 -80.8935992766299,46.42765812485277,0 11.69.2 0 -80.88719358526573 46.42402285548038 0 304.4656588400667 6.67805848190081e-011 0.05089261615147957 relativeToGround #msn_ylw-pushpin_copy:0_copy42001111 -80.88733805785317,46.42398113273752,0 11.69.3 0 -80.88372571725881 46.42182790922119 0 1016.45865451003 6.14644753246544e-011 0.0100106418220931 relativeToGround #msn_ylw-pushpin_copy:0_copy47211 -80.88291598340332,46.42095705507099,0 11.69.4 0 -80.87384037643159 46.40367978785379 0 1016.458654510737 2.158769983942925e-011 0.01717100113822962 relativeToGround #msn_ylw-pushpin_copy:0_copy40100130 -80.87382107768987,46.40372631264508,0 11.69.5 0 -80.87840015983673 46.40930622519564 0 843.7741058018411 0 0.057262293526703 relativeToGround #msn_ylw-pushpin_copy:0_copy3500000 -80.87750573267677,46.40804204270062,0 Long Lake 0 Long Lake 0 -81.00650080174695 46.40908321533048 0 3081.544622196102 4.413000236072347e-010 -0.1065209261795987 relativeToGround #msn_ylw-pushpin3200 -81.0149699680011,46.40683522367214,0 Fueten & Richmond, 1997, Fig 2 - Map of Long Lake region 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Fueten/fueten2.jpg 0.75 46.48990564349332 46.26642898306074 -80.92561465904278 -81.17286370222774 0.913585399369984 Fueten & Richmond, 1996, Fig 7 - ACF axial ratios 0 Grain shape analysis using the autocorrelation funtion (ACF). Symbols scaled accoridng to average grain size. For samples with an axial ration greater than 1.3, the trend and plunge of the long axix are indicated. The trend is constrained by the orienation of the thin section and not by the ACF analysis. 3 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Fueten/fueten7a.jpg 0.75 46.49338843155135 46.29813673518197 -80.92714369372845 -81.18103021043184 Fueten & Richmond, 1996, Fig. 5 - Quartz C axis fabrics 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Fueten/fueten5.jpg 0.75 46.49184923447923 46.28726209190073 -80.92643514291743 -81.17609688655682 Fueten & Richmond, 1979, Fig 4 - Sudbury breccia 0 2 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Fueten/fueten4.jpg 0.75 46.49145299374119 46.31107465414176 -80.9283649314917 -81.17588246293488 Markstay 0 G75 22a Sudbury diabase, composite dike 0 -80.54613055048776 46.48003252008554 0 1014.36259101415 0 0.2262366400018751 relativeToGround #msn_ylw-pushpin_copy1112103 -80.5460842967975,46.48137895924272,0 North Shore - Killarney - Key Harbour 0 Davidson and Bethune, 1988, fig2 0 7dffffff http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Davidson/Killarney_Tyson/davbeth88fig2.jpg 0.75 46.09173572179669 45.89014262730408 -81.1346501971653 -81.59013476568609 -3.86751948543885 Davidson and Bethune , 1988, fig4 0 66ffffff http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Davidson/Killarney_Tyson/davbeth88fig4.jpg 0.75 46.06514984692107 45.86219446446266 -80.54658595047273 -81.00613409731339 -3.419492159614806 Davidson and Bethune, 1988, fig3 0 3dffffff http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Davidson/Killarney_Tyson/davbeth88fig3.jpg 0.75 46.07869154319415 45.87511326784958 -80.8430509488084 -81.29842255071955 -3.478366896156435 Tyson Lake 0 Maps 0 1 Killarney - Tyson Lake 0 1 Maps 0 1 Krogh 1994 fig 2 Grenville Front age map Killarney region 0 Concordia diagram for zircon (2), Monazite (1), and titanite (10) samples; Krogh 1994, Tectonics, 13, 4, p. 971. http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Krogh1994%20fig%204.jpg Location map for samples collected by Haggart et al., 1993 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Haggartsamploc.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Krogh1994%20fig2.jpg 0.75 46.13603973695459 45.89671607619479 -81.046798537973 -81.33457367190141 Bethune, K., 1997 fig 3 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune97fig3.jpg 0.75 46.17970070199822 45.95160012273591 -80.94716452854526 -81.27414964382626 -1.026769424601617 Bethune, K., 1997, fig 7 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune97fig7.jpg 0.75 46.11272420560801 46.06207712795727 -81.03915477795721 -81.14410226504339 -1.277487526342803 Bethune, K., 1997, fig 4 0 4fffffff http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune97fig4.jpg 0.75 46.16768800217317 46.08890641964801 -80.99769429195396 -81.18715984717601 Bethune, K., 1989, Fig 2. 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Bethune89fig2.jpg 0.75 46.13641606885498 46.11648302795475 -81.08044403565488 -81.13213512095612 -0.1279130080116485 Beth_David88Fig2 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Bethune/Beth_David88Fig2.jpg 0.75 46.17675389691569 46.01590595950245 -80.94567026505334 -81.27378190588482 Tyson Lake 0 -81.10445876784779 46.12844399404477 0 6788.901431588385 0 -0.1057009544808591 relativeToGround #msn_ylw-pushpin_copy:0_copy15110010 -81.11842827414307,46.11564542025047,0 K72 1(TS G1- 60-65) 0 -81.1491941716787 46.10907183876987 0 1721.404462248627 1.048233427889532e-009 -0.4171067467590123 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy300002 -81.15003621949418,46.10885369988796,0 Frarey's unit 5, Meta-conglomerate 0 -81.14719032892681 46.10796907420419 0 835.1161273812564 1.046871996702954e-009 -0.4156577437839736 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy100102 -81.14914715023143,46.10828142989696,0 TL78 6a,b; K72 6b - Frarey's unit 3, aluminous? meta-quartzite 0 -81.14057160756167 46.08563185045269 0 1721.404462250041 1.060007992985135e-009 -0.4108914328175949 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy61102 -81.14491204887798,46.0878503677346,0 K72 6a Frarey's unit 1, layered gneiss 0 -81.14844146449275 46.08638633328489 0 284.5857017822654 1.176406009523346e-009 -0.4165608003205017 #msn_ylw-pushpin_copy:0_copy:0_copy1101000 -81.14844146449275,46.08638633328489,0 K72 2a paraschist (TS G1-67, 1756); Sud. Diab.; K72 2b (TS G1-16, 1757), Sud diab dikelet w. garnet bearing chilled margin 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/TS/K722b-1.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/TS/K722b-2.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/TS/K722b-3.jpg -81.10822679394914 46.14265768052554 0 560.7450940047403 0 -0.180064679063938 relativeToGround #msn_ylw-pushpin_copy18200 -81.10978770163956,46.14255520204231,0 K72 3, ductile folded gneiss 0 -81.11255138492815 46.12544331040805 0 174.0895659873205 0 -0.1831811481631508 relativeToGround #msn_ylw-pushpin_copy3004010110 -81.11261963159708,46.12528263957217,0 Sudbury diabase K72 4 (TS G1-17, P1-22) 0 -81.10504054935446 46.12561890874542 0 1217.30874036507 0 -0.1777670437998052 relativeToGround #msn_ylw-pushpin_copy:0_copy761010 -81.10682493323606,46.12398316329046,0 K72 5, Mylonitized granite 0 -81.10420536197427 46.12041955870173 0 477.3610228614695 0 -0.1771654060648772 relativeToGround #msn_ylw-pushpin_copy5002001 -81.10508689796058,46.12015856949435,0 Sudbury diabase, S end of Killarney lake 0 -81.35596534819023 46.04787706884646 0 448.7164014461778 1.934782058831377e-011 -0.1579127086145958 relativeToGround #sn_ylw-pushpin_copy:0_copy531000 -81.35719956969537,46.04781758226927,0 KA78 1 Sudbury diabase, Kakakise Lake 0 -81.34140223612479 46.05051227602177 0 505.8750775612118 1.980092885451655e-011 -0.1474282348703538 relativeToGround #sn_ylw-pushpin_copy:0_copy60101 -81.34147182908662,46.0495258921712,0 Timmins Creek, Street Township 0 Crerar 0 -80.56622442367043 46.63159422785702 0 1198.344938867827 0 0.1168525396198789 relativeToGround #msn_ylw-pushpin6_copy00030 -80.56880366948258,46.63154295609915,0 Maps 0 1 Easton et al., 1999, Fig 6, Ess Creek Fault 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Timmins_Creek/Timmins_Creek.rtf 1 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Easton99fig6.jpg 0.75 46.62687052549315 46.60752142782108 -80.56231740037511 -80.60904115989587 1.246773339584019 Murphy, E. 1999 0 1 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Murphy,%20E.,%201999.jpg 0.75 46.62566956219187 46.60033882195285 -80.55689151239619 -80.59978911922322 -11.50370171336437 Street 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/street.jpg 0.75 46.65441548032153 46.52882828711476 -80.56208696804411 -80.70046685826577 Stops 0 Ess Creek fault 0 -80.58049560704799 46.61635575811877 0 3152.166161209648 3.022605974088537e-011 0.002786150253025141 relativeToGround #msn_ylw-pushpin_copy1300501 -80.58097779752178,46.6190270484994,0 Mississagi Fm - A-1b 0 GE - 530610E, 5162103N WGS84 Stop A-lb. Stop A-lb is the first outcrop to the south abutting the rail line. Alternate Stop A-lb: Mississagi Formation sandstone and semi-pelite interbeds, Southern Province [17T, 530620E, 5161875N] As was the case for Stop A-la, this stop shows typical buff weathering Mississagi sandstone with occasional beds of fine-grained, brown-weathenng siltstone to subarkose. The beds trend 330°, dipping 75° to the northeast. Cross-bedding in the sandy beds also indicates facing to the northeast. The Grenville Front boundary fault trends east in this area, and lies roughly 300 m south o-f the rail line, beneath Timmms Creek. Despite the proximity to the Grenville Front boundary fault, no obvious Grenvillian metamorphic overprint or deformation is observed in this outcrop. Return to vehicles, and continue east another 400 m to Stop A-2, which consists of rock cuts on both sides of the rail line. A parking pullout is present 50 m east of the rock cut on the north side of the right-of-way. -80.59559181179849 46.61154375203078 0 1670.007553832006 2.771131722243457e-011 -0.008184150481598176 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy381020 -80.60019802437726,46.61175051491134,0 Sheared Mississagi - A-2 0 GE - 531310E, 5162431N WGS84 Stop A-2: Sheared Mississagi Formation sandstone and semi-pelite interbeds, Southern Province (96RME-0092) [17T, 531400E, 5162120N] We are still in the Mississagi Formation at this outcrop, however, the sandstone beds are more deformed than at the previous stop, only a few hundred metres to the west. Compare and contrast this outcrop with Stops A-la or A-lb. Cleavage in the outcrop trends 050°, dips 70° southeast, and is subparallel to parallel to bedding. Cross- and graded-bedding, most readily seen on the surface of the north rock cut, indicates facing to the northwest, hence the beds are overturned. Note the presence of generally shallow, southwest-plunging, folds in the cleavage plane. These folds are most readily visible on the northern vertical face of the roadcut. In thin section, the sandstone at this locality is more recrystalhzed than at Stop A-lb; exhibiting a greater proportion ofchlonte-quartz-feldspar matrix, and containing strained quartz and feldspar. Although recrystallized, there is no mineralogical evidence (such as the development ofbiotite), that suggests metamorphic grade at this stop is any different than the grade observed at Stop A-lb. This outcrop lies either on the trace of, or only a few tens of metres north of the Ess Creek fault, a major fault that subparallels the Grenville Front boundary fault from Kukagami Road to River Valley, some 50 km to the east. The location of the rail right-of-way follows an erosional valley developed along the fault trace. Thomson and Card (1963) described the presence of extensive shearing in outcrops adjacent to the fault east ofCrerar, and also report an increase in quartz veining and shearing in an east-west direction in rocks present south of the fault. Thomson and Card (1963) reported that the fault plane dips south at 60° to 80°, and suggested that the fault is north-side down, based on the absence of the Mississagi Formation south of the fault in the Washagami area. Return to vehicles, continue east along the right-of-way from the parking pullout 2.65 km to the next stop, which is a rock cut abutting the south side of the rail line. Additional exposures of gabbro are present a few tens of metres into the bush. -80.58049560704799 46.61635575811877 0 3152.166161209648 3.022605974088537e-011 0.002786150253025141 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy470011 -80.59105557862951,46.61467693966819,0 Amphibolite schist (metavolcanic) - A-4 0 GE - 532086, 5162693N WGS84 Stop A-4: Thinly layered amphibolite schist. Transition Zone (E-3004, 96RME-0123, -0447) [17T, 531930E, 5162560N] We are now south of the Ess Creek fault, in the area marked as Transition Zone in Figure 3. As we look at the rocks between Stops A-4 and A-ll, items to consider and observe at each outcrop include the following: 1) what is the metamorphic grade of the unit? 2) is the unit a metamorphosed part of the Huronian Supergroup or does it belong to a different rock sequence? 3) what is the deformation state of the unit? and 4) are the rocks in the Transition Zone part of the Southern or the Grenville provinces, and where would you put the Grenville Front? The first unit we encounter south of the Ess Creek fault forms a prominent east-trending ridge. The north-facing slope of this prominent ridge provides typical exposures of a thinly layered, amphibolite schist unit. This ridge can be traced to the east for at least 2 km, where more massive amphibolite units are present. The unit also can be traced in drill core for another 3 km to the west beneath the swamps along the banks of Timmins Creek, although it is offset by northwest-trending faults (Maclean 1983). Lumbers (1973) mapped these rocks as being of volcanic or volcaniclastic origin, and in his map legend, included them in the Mississagi Formation; however, he provided no explanation of why he did so. The layering in these rocks reflects distinct mafic (amphibole - chlonte - plagioclase ± epidote) and mesocratic to leucocratic (quartz - plagioclase - epidote) variations in composition. Garnet is locally present in more massive amphibolite layers in outcrops farther east. Tight S- and Z-shape folds are present, as well as isoclinal folds, with axial planes parallel to the main foliation. Locally these rocks could be classified as blastomylonite. Compare the strain of these rocks with the rocks we saw at Stop A-3b. The geochemistry of several samples of this unit, collected from near this outcrop and farther east along strike suggests a similarity with mafic metavolcanic rocks of the Stobie Formation (Easton 1998) (compare samples 96RME-0123, -0447, -3004 and 86RLD-1902, Table 2). Murphy (1999) obtained a hb-pl temperature of620°C (Pof 6 kb, Holland and Blundy 1994) from this outcrop, suggesting middle amphibolite conditions, consistent with the observed mineral assemblages. In the short-distance from the right-of-way, we have gone from lower greenschist to middle amphibolite facies. Proceed approximately 50 m south-southwest to the next outcrop area. -80.58243153923294 46.61256914183166 0 1100.00644683505 2.536320826695686e-011 0.001379109606200944 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy32000 -80.58089428678814,46.6170900295203,0 Deformed psammite - A-5 0 GE - 532061E, 5162587N WGS84 Stop A-5: Deformed psammite and pelite, folded quartz veins, Transition Zone [17T,531975E,5162365N] This small outcrop contains a contact between a psammitic and a pelitic unit, both of which contain several folded quartz veins. Are these rocks less or more strained than those we saw at Stops A-3b and A-4? Could these rocks be Huronian metasedimentary rocks? To the east, these are overlain by a felsite containing elongated, felsic, clasts 1.5-2 cm wide and up to 50-70 cm long. This felsite unit was interpreted to represent a felsic pyroclastic unit (Easton et al. 1996, Murphy 1999). Geochemically, the felsite resembles dacitic rocks from the Stobie Formation (compare samples 96RME-0124 and 86RLD-0203, Table 2). Further, the chemistry of this felsic unit resembles that of granitoid rocks we will see at Stops A-8 and A-13 (see also Easton 1998), which yielded a U-Pb zircon age of2460+/-20 Ma (Table 1), consistent with correlation of this unit with the Stobie Formation. Proceed approximately 95 m south across the alder swamp to the prominent ridge. As you climb up onto the ridge, you will encounter a north-facing outcrop scarp. Examine stripped outcrop along this scarp. -80.58243153923294 46.61256914183166 0 1100.00644683505 2.536320826695686e-011 0.001379109606200944 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy3412 -80.58121106818355,46.61609331247215,0 Polymict cong. - A6 0 GE - 532072E, 5162521N WGS84 Stop A-6: Polymict conglomerate and quartz veins. Transition Zone (E-3005) [17T, 532000E, 5162270N] The north-facing scarp exposes one of the few conglomerate units in the transition zone. This polymict conglomerate unit is at least 75 m thick, and contains a few, thin, schistose quartzite interbeds. Several large quartz veins cut the outcrop and tend to obscure some of the features present in the conglomerate. These veins are folded and exhibit the same fold geometry as the veins seen at Stops A-4 and A-5. Murphy (1999) described quartzite, granite and metavolcamc fragments from this unit. The matrix is varied both in grain size (medium- to coarse-grained) and composition (quartzofeldspathic to amphibole-rich). Five- to 8-mm-size garnets are common in the matrix, and exhibit pressure-shadows but no obvious internal rotation. Bedding (So) between the conglomerate and the quartzite beds trends 050° and is slightly discordant to the foliation in the unit (S1) which trends 060° and dips 60° to the southeast. The conglomerate clasts are generally elongated into the plane of the foliation. Murphy (1999) has suggested that this conglomerate may be correlative with the Ramsey Lake Formation, in part because of the gradational contact with the overlying garnet-biotite schist. Geochemistry (sample 96RME-3005, Table 2) on the matrix of the unit is inconclusive with respect to stratigraphic assignment. Metamorphic grade in this unit is lower to middle amphibolite facies. Murphy (1999) obtained TWEEQU determined P and T values of 6.7 kb and 630°C, respectively, from this outcrop. The gt-bi thermometer of Hodges and Spear (1982) gave a similar T of 637°C (at 5.5 kb) (Murphy 1999). As a historical note, Fairbairn (1939) reported deformed granitic pebbles in pink and grey, "Late Precambrian (i.e., 'Killarnean') gneisses" present at this locality. These rocks lie within a zone which he interpreted as representing metamorphosed and "granitized" Huroman sedimentary rocks. The metaconglomerate is overlain by a schist unit with very distinctive geochemistry, which can be traced along strike to the east (e.g., sample 96RME-3031, Table 2). characterized by a low LaN/Yb^ ratio, a prominent positive Eu anomaly (Eu^/Eu^* = 1.72), and higher iron content. Similar chemical signatures have only been observed in fine-grained subarkosic samples from the Mississagi Formation (e.g., sample 86RLD-3902, Table 2, and unpublished data by C. Fedo, written communication, 1998). These unusual patterns are similar to those reported for the Levack gneiss. Consequently, these sediments may be the result of a significant influx of detritus from the Levack gneiss complex located to the northwest. Proceed approximately 125 m east to the next outcrop area. -80.58424977630948 46.61458479869977 0 2262.192938458904 5.315288780284809e-011 5.761927759026511e-005 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy350130 -80.58116777927572,46.6154815383818,0 Nipissing - A-7 0 GE - 532133E, 5162501N WGS84 = 532123E, 5162493N NAD27 Stop A-7: Schist, breccia and Nipissing gabbro, Transition Zone (E-3006) [17T, 532125E 5162270N] A variety of features are present in the rounded outcrops at this stop. Medium-grained relict ophitic-textured amphibolite, correlated with the Nipissing gabbro on the basis of texture and chemistry (sample 96RME-3006, Table 2), cuts metasedimentary rocks composed of garnet-biotite schist, quartzite, and a clast-supported breccia that contains subangular granite cobbles texturally similar to granitoid rocks that we will see at Stop A-8. Unfortunately, the quality of the exposure here is not good enough to determine if the sequence here lies unconformably atop the granitoid rocks seen at Stop A-8, or whether the breccia is the result of intrusion and/or tectonism. The Nipissing gabbro exposed here is part of a much larger body that continues farther east and south (Figure 3). Murphy (1999) obtained TWEEQU determined P and T values of 7.5 kb and 655°C, respectively, from garnet-biotite schist from this outcrop and a gt-bi temperature of637°C (at 5.5 kb; Hodges and Spear 1982). Proceed approximately 60 m southwest to the next outcrop area. -80.58424977630948 46.61458479869977 0 2262.192938458904 5.315288780284809e-011 5.761927759026511e-005 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy36121 -80.580357408662,46.61521641427417,0 Foliated Granite - A-8 0 GE - 532134E,5162410N WGS84 Stop A-8: Foliated granite unit, Transition Zone (C-96-7, E-3008) [17T, 532030E, 5162215N] This outcrop exposes a homogeneous, foliated, granodiorite to monzogranite. Contact relationships with the metasedimentary units seen previously at Stops A-6 and A-7, and at the next two stops, are not exposed, expect perhaps at the last stop. However, the map pattern of this granitoid unit is discordant with respect to the trend of the metasedimentary rocks (Figure 3). A sample from this outcrop yielded a U-Pb zircon age of 2460 ± 20 Ma and a poorly constrained, upper intercept, metamorphic titanite, age of 1720 Ma (Table 1) (Corfu and Easton, in press). Zircon overgrowths or metamorphic titanite ofGrenvillian age were not recovered from this sample, which is located only 150 m north of the GFBF. We will see the deformed equivalent of this rock within the Grenville Province at Stop A-ll. The granitoid at this outcrop is geochemically similar to felsic metavolcanic rocks present stratigraphically and structurally beneath the metasedimentary rocks (e.g. sample 96RME-0124, Table 2) as well as migmatitic granitoid orthogneiss present south of the GFBF which we will examine at Stop A-13. The felsic metavolcanic rock is chemically similar to dacitic rocks of the Stobie Formation near Sudbury (Easton 1998), and both the dacitic and granitoid rocks have the geochemical characteristics of Fill rhyolite (e.g., Zr/Y ratios of 5 to 7.5, Zr 280-790, Y 42-110, TiC>2 0.3-0.8, Sc 6-12, Sr 110-210, and elevated, flat REE patterns with negative Eu anomalies). Volcanogenic massive sulphide deposits are commonly associated with supracrustal sequences containing Fill-type felsic volcanics and subvolcamc intrusions. Proceed approximately 75 m southwest to the next outcrop area. -80.58424977630948 46.61458479869977 0 2262.192938458904 5.315288780284809e-011 5.761927759026511e-005 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy3711 -80.58040079118602,46.61448191406691,0 Staurolite-garnet schist - A-9 0 GE - 532013E, 5162293N WGS84 Stop A-9: Staurolite-garnet-biotite schist, fold style, garnetiferous mafic dyke. Transition Zone (E3013) [17T, 531880E, 5162130N] This stop consists of several closely-spaced outcrops. The purpose of this stop is to observe the changes in bedding/cleavage relationships related to folds present in this outcrop area and in Stop A-10. These relationships are illustrated in a generalized fashion in Figure 7. Compositional layering (bedding) is discernible in the outcrop as variations in garnet, biotite and muscovite content between different layers, overall, the rocks are pelitic to semi-pelitic in composition. No obvious facing criteria are preserved in this unit, which hampers structural and stratigraphic analysis at a larger scale. The map pattern shown in Figure 3 suggests we may be located near a larger-scale, northwest-trending cross-fold that warps the generally homoclinal succession present in the transition zone. At the northwest portion of the outcrop area, we see Sj (050°/650) cuts bedding (So, 330°/80°) at a high-angle, whereas in the central part of the outcrop area, Si is subparallel to (So). This suggests that S1 is axial planar. In the east-central part of the outcrop area, a fine-grained mafic dyke, containing cross-shaped garnet porphyroblasts, cuts thin, quartz-rich layers within the biotite schist unit. As shown in Figure 7, these folded layers appear to be related to the larger fold on the outcrop. This suggests that folding occurred prior to peak metamorphism. This is consistent with the lack of inclusion-trails in garnets, and the lack of other syn-deformational features in the biotite schist unit. Proceed approximately 80 metres south to the next outcrop area. -80.5828022118325 46.61340628881774 0 929.577655221236 7.338955598010613e-012 0.001109626409946199 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy29012 -80.58181421418645,46.61343656899896,0 Kyanite - A-10 0 GE - 531942E, 5162216N WGS84 Stop A-10: (kyanite)-staurolite-garnet-muscovite-biotite schist, bedding, fold style, Transition Zone (C-96-6, E3012, 96RME-0234) [17T, 531900E, 5162050N] As in the case of Stop A-9, this stop consists of several closely spaced outcrops where we can observe bedding/cleavage relationships similar to that observed at the last stop, and illustrated in Figure 7. The main difference here is that we are in a slightly different compositional unit, as we now observe the assemblage kyanite-staurolite-garnet-muscovite in these schists. In terms of geochemistry, the schists at this locality are most likely correlative with the Pecors Formation of the Huronian Supergroup (compare samples 96RME-0234, -0242, and 86RLD-3703, -5102, Table 2). Murphy (1999) obtained TWEEQU determined P and T values of 7.6 kb and 678°C, respectively, from this outcrop and a gt-bi temperature of690°C (at 8.0 kb, Hodges and Spear 1982). In addition, Corfu and Easton (in press) used monazite to date the timing of metamorphism in this schist at 987+/-3 Ma (Table 1). This is a Grenvillian age, and given the similarity in metamorphic conditions reported by Murphy (1999) between Stops A-4 to A-10, suggests that all the rocks in the Transition Zone have been affected by Grenvillian metamorphism. It is also the same as a U-Pb zircon age obtained by the Geological Survey of Canada (unpublished) from an undeformed pegmatite 5 km south ofWahnapitae village. Lithologically, however, the rocks within the transition zone have either been correlated with the Huronian Supergroup (Fairbairn 1939; Lumbers 1973; Easton et al. 1996; Murphy 1999) or placed in a transitional category, belonging neither to the Grenville or the Southern Province (e.g., Collins 1913, Thomson 1961, Thomson and Card 1963). Proceed approximately 30 m west-southwest to the next outcrop. -80.58189113851969 46.61339600749247 0 593.4458921880654 0 0.001771756216986852 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy451030 -80.5828083849769,46.61270762638836,0 Gren. Front Bound. Fault - A-11 0 GE - 532049E, 5162242N WGS84 Stop A-11: Fault gouge associated with the Grenville Front boundary fault, Transition Zone (E-3036) [17T, 531870E, 5162055N] This outcrop lies along the trace of the Grenville Front boundary7 fault (GFBF), as mapped by Lumbers (1973). Hematized and chlontized fault gouge, similar to that found in this outcrop is a common feature observed along the GFBF east ofSudbury; for example, similar rock can be found on small islands in the Wanapitel River along the trace of the GFBF. Here, the fault gouge is likely derived from granitoid rocks similar to those seen at Stop A-8, based both on preservation of textures in lower strain domains, and whole-rock geochemistry (96RME-3026, Table 2). North of this outcrop, at Stops A-4 to A-10, we examined a moderately deformed amphibolite-grade sequence of supracrustal rocks, which locally preserves bedding features. Southof this outcrop, at Stops A-12 to A-15, we will see that the rocks become increasingly migmatized, that compositional layering is increasingly transposed, that syn- and late-tectonic pegmatite veins become abundant, and that the protoliths of the gneissic rocks becomes increasingly obscure. As has already been noted in the introduction, thermobarometry indicates only a modest change in temperature (up to 50°C higher south of the GFBF, but the temperature determinations are within the error limits of the methods) and pressure (up to 1 kb higher south of the GFBF, again within error limits). In addition, U-Pb geochronology (Corfu and Easton in press) indicates the development ofmetamorphic monazite at 989 ± 4 Ma both north and south of the GFBF, suggesting that in the Timmms Creek area, the GFBF does not coincide with the northern limit of Grenville metamorphism. Proceed approximately 85 m southeast to the next outcrop -80.58110752872385 46.61299188758784 0 523.5404985445422 1.95584246325349e-011 0.002341238908240271 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy3920 -80.58144707087703,46.6129816063595,0 Staur.-kyanite-garnet-biot. gneiss (zircon, 992 Ma; monazite, 989 Ma); 685C, 8.1 kb - A12s 0 -80.58158019165212 46.61115090673753 0 519.6526754795849 1.955841269778055e-011 0.0019977066761354 relativeToGround #msn_ylw-pushpin_copy117010 -80.58260225731353,46.61129066636503,0 Folded gneissosity - A12 0 -80.58079740720572 46.61257263514665 0 521.7394080859834 0 0.002566598841439403 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy441 -80.5818357791013,46.61236347834566,0 Migmatitic granite gneiss - A13 0 GE - 531984E, 5161983W WGS84 Stop A-13: Migmatitic granite gneiss unit, Grenville Province (E-3026) [17T, 531940E, 5161800N] This migmatitic granitoid gneiss is typical of several orthogneiss bodies that lie within the GFTZ east ofSudbury. Similar rocks will be seen at Stops B-6, B-7 and B-10, farther to the southwest. Orthogneiss from this outcrop and from others along strike in this unit are geochemically similar to the non-migmatitic foliated granite seen at Stop A-8, dated by Corfu and Easton (in press) at 2460 ± 20 Ma. The unit seen at Stop A-13 can also be correlated on the basis of lithology and chemistry with another orthogneiss body exposed 7 km to the south-southeast in Street Township, which also yielded a U-Pb zircon age of2475+25/-10 Ma (Corfu and Easton, in press). In addition, both the granite at Stop A-8 and the dated orthogneiss body in Street Township contain discordant metamorphic titanite which gave an imprecise upper intercept age of 1720+36/-19 Ma. The errors on the titanite age overlap the age range of Killarnean magmatism to the southeast (1750-1730 Ma) and the development of hydro thermal monazite at 1700 ± 2 Ma within the Huronian Supergroup only 10 km north of this outcrop (Schandl et al. 1994). Proceed approximately 135 m south-southeast to the next outcrop area. -80.58172048146165 46.61163862655018 0 520.3993840496954 1.955841499000908e-011 0.001895777982515613 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy410000 -80.58222541673023,46.61068994296878,0 Mafic gneiss & pegmatite - A14 0 GE - 532035E, 5161892N WGS84 Stop A-14: Mafic gneiss, pegmatite, Grenville Province (E-3027) [17T, 531975, 5161665N] This large outcrop area illustrates the appearance of typical migmatitic garnet-amphibolite in the area. The outcrop is invaded by large masses of coarse-grained syenogranitic pegmatite, with biotite becoming more abundant in the amphibolite adjacent to the pegmatite. Murphy (1999) obtained a hb-pl temperature of730°C (at 8.3 kb, Holland and Blundy 1994) from this outcrop. Mafic gneiss near Stop A-12 and at this outcrop (samples 96RME-3020, -3027, and -3127, Table 2) have a different geochemical signature to the amphibolite at Stop A-4, and to Nipissing gabbro. To date, no satisfactory assignment of the mafic gneiss to any particular suite has been established (cf., Easton and James 1997) — they are not obviously related to either the Huronian Elsie Mountain and Stobie formations, nor are they related to the East Bull Lake metaplutonic rocks or the Nipissing gabbro suite. It is possible they could be Archean in age, but this is speculative. Rocks of this chemistry are not seen north of the GFBF in the transition zone. The occurrence of chemically distinctive mafic and quartzofeldspathic gneisses south of the GFBF (e.g., Stop A-15) contrasts with the local presence of rocks that are similar to those present north of the GFBF (e.g., sample 96RME-0242, Stop A-12; Huronian granites, Nipissing gabbro and EBLI suite rocks elsewhere in Street Township). One explanation is that we are seeing a somewhat deeper structural level exposed south of the GFBF, where we are seeing the relicts of younger intrusive rocks (Nipissing and EBLI suites) that were intruded into Superior Province basement, perhaps at or below the Huronian unconformity. Proceed approximately 70 m south to the next outcrop area. -80.58103441043703 46.60984873549513 0 515.2843497045136 0 0.002394291505913695 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy4000 -80.58162292885174,46.60983864349415,0 Musc.-biot. paragneiss, quartzose gneiss, folded mafic dikes, garnet amphibolite gneiss (pillowed?) - A-15 0 -80.58103441043703 46.60984873549513 0 515.2843497045136 0 0.002394291505913695 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy42000 -80.58160221442122,46.60916618790719,0 Tomiko 0 -79.40849017153724 46.56732496843926 0 1997.467466941931 8.933811687102161e-013 0.000689025337143209 relativeToGround #msn_ylw-pushpin05200 -79.41044054258194,46.56754844837257,0 Wanapitei-Dryden Rd 0 Maps 0 1 Easton et al., 1999, Fig, 10. 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Easton99fig10.jpg 0.75 46.51235307889347 46.49568649908667 -80.67067607716427 -80.71539834403984 1.614087466212376 G75 6, unit 21 (Burwash sheet) 0 -80.70077994259393 46.48584607682994 0 7151.587671914288 2.132549061123456e-011 0.1140638084498993 relativeToGround #sn_ylw-pushpin_copy:0_copy67100 -80.71626116292045,46.48787725480277,0 Deformed Sudbury diabase 0 -80.72748410873845 46.49935156776829 0 3235.230035941535 3.440893094972647e-011 0.09471791870797579 relativeToGround #msn_ylw-pushpin_copy:0_copy681000 -80.72631164741145,46.50123314041783,0 Deformed Sudbury diabase 0 -80.72748410873845 46.49935156776829 0 3235.230035941535 3.440893094972647e-011 0.09471791870797579 relativeToGround #msn_ylw-pushpin_copy:0_copy5900004 -80.73129352326666,46.50005399879213,0 Deformed Sudbury diabase 0 -80.71705252873468 46.49556021900186 0 3235.230035944364 3.440893094971465e-011 0.1022834363818852 relativeToGround #msn_ylw-pushpin_copy:0_copy6510 -80.73149508024079,46.49640217929333,0 Sudbury diabase G75 21a (TS G1-34); cutting 'River Valley' anorthosite 0 Garnet diabase dike cutting Red Deer anorthosite NE corner of Clelland Township; no apparent deformation; diabasic texture preserved; plag. recrystallised with cloudy relict cores but not polygonized; pyroxenes partly to totally polygonized or converted to granular masses of amphibole; some amphibole coronas; garnet rich -80.69814908638828 46.44784451685589 0 1671.40299549494 0 0.1147033347146785 relativeToGround #msn_ylw-pushpin_copy:0_copy82000 -80.70037107062206,46.44744315365261,0 Wanapitei Complex 0 Maps 0 1 Easton et al., 1999, Fig. 14 Wanapitei complex 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Easton99fig14.jpg 0.75 46.48213807935763 46.46784470901705 -80.79823389899988 -80.82728229106891 -1.055779372440777 W78 1 metadiabase 0 -80.82384008066472 46.45220982946493 0 3235.230035944364 1.56093987899658e-011 0.02484354112537478 relativeToGround #sn_ylw-pushpin_copy:0_copy7100110 -80.82273486914059,46.45180752475285,0 W78 2 Fresh Grenville? diabase 0 -80.81980161023689 46.45678938691195 0 2487.296596158044 0 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#msn_ylw-pushpin_copy2190111211 -81.74801418294908,46.0947425751193,0 Plane_Table_Lake 0 F1 folds cut by F2 foliation 0 -81.71178068023464 46.10139646757351 0 199.953053828104 3.975772072747703e-010 -1.194061948777417 relativeToGround #msn_ylw-pushpin_copy5 -81.71183020154935,46.10115002547575,0 F1 folds (s) 0 -81.71322626778712 46.09940471235922 0 106.4444834961484 0 -1.195156571519101 relativeToGround #msn_ylw-pushpin_copy101 -81.71328064038971,46.0993949757414,0 F1 fold (s) 0 -81.71421282942158 46.09956974614956 0 107.4446104881805 0 -1.195867432616703 relativeToGround #msn_ylw-pushpin_copy110 -81.71416899040902,46.09959004334323,0 F1 folds (s) 0 -81.71547724948808 46.09958150285942 0 106.4445928610298 1.349730204501555e-010 -1.196778504151193 relativeToGround #msn_ylw-pushpin_copy811 -81.71550819264132,46.09960053386662,0 Plane Table Lake, 46.1004, -81.7136 0 -81.71348298448999 46.10042000627515 0 74.86832265982213 0 -1.195341471583509 relativeToGround #msn_ylw-pushpin_copy130 -81.71356874264887,46.10041688842278,0 Geology 0 1 Espanola Fm 0 -81.71637796402506 46.09432667850563 0 506.6892410374686 4.772961938591136e-010 -1.197366765574046 relativeToGround #msn_ylw-pushpin_copy00 -81.71727605053032,46.09405472161016,0 Bruce cong. 0 -81.71637796402506 46.09432667850563 0 506.6892410374686 4.772961938591136e-010 -1.197366765574046 relativeToGround #msn_ylw-pushpin_copy30 -81.7174513168393,46.09385609180475,0 Boundaries 0 Untitled Path 0 #msn_ylw-pushpin_copy225 1 -81.71696901908803,46.09758625643303,0 -81.71688617406248,46.09757391316688,0 -81.7163549973836,46.09754521746132,0 -81.71594610733632,46.09753523987998,0 -81.7158434105325,46.09753369894851,0 -81.71471770653376,46.09740237776035,0 -81.71434791337221,46.09742650163322,0 -81.71411890488528,46.0974063838483,0 -81.71364873188792,46.09744873474886,0 -81.71326302487867,46.09741281414604,0 -81.71252486290781,46.09745350037497,0 -81.71051277239698,46.09778731200876,0 Untitled Path 0 #msn_ylw-pushpin_copy41 1 Untitled Path 0 #msn_ylw-pushpin_copy10 1 -81.71600692878155,46.10071432749372,0 -81.71594879549876,46.10077761645913,0 -81.71390637089627,46.10122314423269,0 -81.71254249822167,46.10150047002775,0 -81.71034782854888,46.10196384043847,0 Untitled Path 0 #msn_ylw-pushpin09 1 -81.71790544395127,46.09801777712335,0 -81.71780065353943,46.09804019366375,0 -81.71318592552098,46.09925923573179,0 -81.70976785771298,46.10017864504299,0 Diabase clasts in Sud. brecc. 0 -81.71201918244246 46.10086361791381 0 198.9654124551408 4.51050688873993e-010 -1.194233803860109 relativeToGround #msn_ylw-pushpin_copy411 -81.71234445476387,46.10101087131095,0 Sud. diab 0 -81.71383541865633 46.10125207740039 0 767.3076894247868 4.40880333035961e-010 -1.195609104887227 relativeToGround #msn_ylw-pushpin_copy78 -81.7129908614659,46.10260961828263,0 Diabase 0 -81.71106931790403 46.10177311963059 0 193.1084548818651 3.627948943419947e-010 -1.196281581947714 relativeToGround #msn_ylw-pushpin_copy93 -81.71150452156479,46.10180968120383,0 Sudbury Diabase 0 Thin section - chilled margin with phenocrysts of plag and olivine http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/SuddiabwhiteFFallsTS.jpg -81.71152679150578 46.10154645231428 0 47.63951623147289 5.255039959552935e-010 -1.193931025164379 relativeToGround #msn_ylw-pushpin_copy7 -81.71149634278567,46.10152643223142,0 Turbidites 0 Turbidites with argillaceous tops containing a crenulation cleavage; the cleavage is developed in association with a mesoscale Z-shaped fold. Diabase seems to terminate on the north side of the larger outcrop. -81.72098568389401 46.10962019705314 0 65.80080280982337 4.73728855401535e-010 -1.200747238405376 relativeToGround #msn_ylw-pushpin_copy20 -81.720915811612,46.10960398681581,0 Gabbro -diabase body 0 -81.72824105127202 46.12068569126897 0 1181.623717192129 4.155351868142576e-010 -1.205975526280813 relativeToGround #msn_ylw-pushpin_copy61 -81.73247637912238,46.11990903944722,0 Transition zone - Tillite to bedded tillite to 1m thick beds of conglmerate 0 -81.71023645663315 46.1021455942935 0 440.6586064292071 3.390096467085627e-010 -1.192963459131267 relativeToGround #msn_ylw-pushpin38 -81.71049009918336,46.10221821303192,0 Coordinate locations 0 444432, 5105581 0 -81.71479652933634 46.10001481499565 0 665.0032537724384 0 -1.196287820028364 relativeToGround #msn_placemark_circle_copy3201121111 -81.71894406945734,46.1015433698522,0 444408, 5105393 0 -81.7191301283429 46.0998715517018 0 90.73916396630976 8.99465350484612e-011 -1.199410397400383 relativeToGround #msn_placemark_circle_copy25021112 -81.71923726298523,46.09984952164387,0 444578, 5105480 0 -81.71665968200662 46.1009262360383 0 469.4114679958672 0 -1.197630289490185 relativeToGround #msn_placemark_circle_copy29012111 -81.71703930460004,46.1006500494624,0 444943, 5105563 0 -81.71240805723474 46.10146431915334 0 204.1715031002731 2.340512897136927e-011 -1.194566977313424 relativeToGround #msn_placemark_circle_copy240213 -81.71232875124011,46.10142232102659,0 444790, 5105417 0 -81.71358747810329 46.10035874731651 0 469.4114679986965 0 -1.195416611129898 relativeToGround #msn_placemark_circle_copy19011112 -81.71430227781245,46.10010125729033,0 444500, 5105237 0 -81.71777045014429 46.0985227292022 0 469.4114679979892 0 -1.198430597875223 relativeToGround #msn_placemark_circle_copy330111 -81.71802051973344,46.09845353221603,0 445035, 5105148 0 -81.71043347842605 46.09803375716527 0 469.4114679972818 3.649875522030605e-011 -1.193144103201511 relativeToGround #msn_placemark_circle_copy260111111 -81.71108757390614,46.09769310068835,0 445021, 5105298 0 -81.71112110293757 46.09916922806914 0 192.9559194269826 9.53450074111698e-011 -1.193639081951413 relativeToGround #msn_placemark_circle_copy3401111112 -81.7112987420002,46.09904433729737,0 445145, 5105441 0 -81.70699000117199 46.10042379626199 0 839.6490305328713 7.255560199733773e-012 -1.190663005530809 relativeToGround #msn_placemark_circle_copy1801223 -81.70970248945525,46.10033956317757,0 Raven Lake 0 Diabase in/"cutting" Sud. Breccia 0 -81.72019299121551 46.18706047019832 0 1300.803767282415 0 -0.04977070686988327 relativeToGround #msn_ylw-pushpin_copy11 -81.72032310393108,46.18709255176803,0 Road to diabase - breccia outcrop on Raven Lake 0 #msn_ylw-pushpin115 1 -81.71609149791043,46.18613549083584,0 -81.71623590681793,46.18619125283002,0 -81.71636330979503,46.18622645028096,0 -81.716770969663,46.18631439221198,0 -81.71700029275846,46.18637598261577,0 -81.71744625651947,46.18654325584963,0 -81.71778609516331,46.18671646701388,0 -81.71844861756188,46.18691594058808,0 -81.72028712868017,46.18710589451176,0 Whitefish Falls to Windy Lake 0 Nairn Centre shatt. 0 -81.57970828970782 46.3415530672428 0 9399.075483670897 3.452833512555569e-012 -0.08285763699378451 relativeToGround #msn_ylw-pushpin_copy3 -81.55545118319002,46.33000112084886,0 Worthington jnct w. 17 0 -81.48099895018818 46.33998169821288 0 6332.989652969168 0 -0.01099085330828305 relativeToGround #msn_ylw-pushpin003 -81.48508013858189,46.33612913620824,0 Worthington 0 -81.4642088369561 46.40293379053814 0 6332.989652972704 2.589742776434118e-012 0.001181661548769296 relativeToGround #msn_ylw-pushpin_copy1051 -81.46629787452248,46.40327828336917,0 turnoff to Windy Lake 0 -81.46575224196616 46.42170370629286 0 12690.03332138352 1.068761939041335e-012 7.602902649415312e-005 relativeToGround #msn_ylw-pushpin_copy01 -81.46575221671365,46.4348190557122,0 Maps 0 Instruct 0 1 Espanola - McGregor Bay 0 http://instruct.uwo.ca/earth-sci/200a-001/dikes1.jpg 0.75 46.246561236962 46.0328317688597 -81.50122341821584 -81.81038987121951 0.9429479557250456 La Cloche syncline 0 http://instruct.uwo.ca/earth-sci/200a-001/howrylake.jpg 0.75 46.16030452990169 46.0861175099253 -81.38743658464678 -81.50004784795874 Bass Lake region 0 1 http://instruct.uwo.ca/earth-sci/200a-001/basslake.jpg 0.75 46.24550817480409 46.15303199349366 -81.7004713789695 -81.81259708484045 0.5742101081807109 Local 0 Bass Lake 0 2 basslake_1.jpg 0.75 46.24533705223337 46.15288773445298 -81.70043587591691 -81.81266626712902 0.7166833185946813 Espanola Cutler Pronto 0 Park vehicles - Pronto Mine 0 -82.71983963154203 46.20888695708489 0 1093.135682934033 6.743673963970641e-023 -1.171123660656236 relativeToGround #sn_ylw-pushpin_copy:0_copy:0_copy770 -82.7203080725604,46.20865716401994,0 Pronto Mine turn off Hwy 17 0 -82.70508588828082 46.20036382228167 0 4697.798338548469 0 -1.160475261411477 relativeToGround #sn_ylw-pushpin_copy:0_copy:0_copy5402 -82.71789290280121,46.19774378589207,0 Maps 0 Local (c:\fieldlog\Huronian_map\) 0 1 North Channel dikes 0 nchanneldikes_1.jpg 0.75 46.741662722663 45.94365428273505 -81.27687463534539 -84.76379487642194 -8.597206065845594 Cutler 0 0218cutler_1.jpg 0.75 46.29594239244394 46.08524671389559 -81.99398736305682 -83.07290384947729 -1.553743812112371 Massey 0 massey1_1.jpg 0.75 46.22607164748135 46.19518834163599 -82.06927556344751 -82.12750088129472 0.483437641163182 instruct 0 1 Massey 0 http://instruct.uwo.ca/earth-sci/200a-001/1494masseybreccf2f3folds.jpg]]> http://instruct.uwo.ca/earth-sci/200a-001/massey1.jpg 0.75 46.22609613838868 46.19511366040637 -82.06919450465861 -82.12753233711339 0.6909352663318785 Cutler region 0 http://instruct.uwo.ca/earth-sci/200a-001/0218cutler.jpg 0.75 46.29603516799352 46.08528917089486 -81.99410715199414 -83.07233834797115 -1.566327475162768 Raven Lake NW-SE t. Diabase 443954E, 5114524N 0 -81.72596700806056 46.18212192412084 0 1023.859019662673 0 -0.05393705988563245 relativeToGround #msn_ylw-pushpin_copy40610 -81.72617863441703,46.18198613327585,0 Anderson Lake shatter cones 0 -81.73370575019575 46.22209991931187 0 959.2864609818099 0 -0.05951875160922279 relativeToGround #sn_ylw-pushpin_copy1122 -81.735238519029,46.22138510790505,0 F3 folds 0 -81.73618006703364 46.22939997414848 0 997.0409050320828 47.35429074587797 -0.3609720524264293 relativeToGround #sn_ylw-pushpin_copy9104 -81.7369740598522,46.22924415384178,0 Cleaved Sudbury breccia 0 -81.73618006703364 46.22939997414848 0 997.0409050320828 47.35429074587797 -0.3609720524264293 relativeToGround #sn_ylw-pushpin_copy13060 -81.73695852087471,46.232602969414,0 Ramsay Lake congomerate 0 -81.76785418601705 46.27774750663657 0 3153.668873303801 0 -0.3716244813974402 relativeToGround #sn_ylw-pushpin_copy123000 -81.76093116123209,46.27910520797078,0 Espanola roadcut breccias 0 -81.77454534251527 46.27837438758812 0 3060.563829628445 0 -0.3764613852181993 relativeToGround #sn_ylw-pushpin_copy0020 -81.77891239587505,46.27805577522492,0 McKim Fm polyphase deformation 0 -81.76785418601705 46.27774750663657 0 3153.668873303801 0 -0.3716244813974402 relativeToGround #sn_ylw-pushpin_copy602 -81.7599195282623,46.2798168680326,0 Massey - polyphase deformed 'Sudbury breccia' and dike 0 -82.10145956988488 46.20485789650947 0 4463.088470711791 0 -0.6246288145619435 relativeToGround #sn_ylw-pushpin_copy808 -82.10250601714037,46.20773933577286,0 Cutler granite 0 -82.45496599629367 46.19970555687323 0 2301.057251447326 0 -0.8700457290924007 relativeToGround #sn_ylw-pushpin_copy2090 -82.45965910818143,46.19964747391275,0 Keweenawan 0 Sudbury to Barry 0 Red Deer lake 0 1 G76 51 marble? 0 -80.73174844769181 46.39355045381799 0 3177.795799644116 3.555116586299368e-011 0.1208597872021444 relativeToGround #msn_ylw-pushpin_copy:0_copy46113 -80.74152095014554,46.39001068796728,0 G76 57 fol. amph. w. stretch. plag conv. grnt 0 -80.64967390655329 46.10420772556791 0 2402.155836805565 2.260890379759044e-011 0.1802102969312304 relativeToGround #msn_ylw-pushpin_copy:0_copy430123 -80.64228279828527,46.10530669170377,0 mutliple dikes - 518717, 5140214 0 -80.75254810837069 46.41339740881168 0 1658.975819369776 3.125792465301296e-011 0.07672593688786759 relativeToGround #msn_ylw-pushpin_copy:0_copy2000000 -80.75625899763085,46.41480025326939,0 Sud diab G75 3 (TS G1-24 = 6735), G72 3 (G1-21 2378 spinel) st ENE-WSW 0 -80.99382498653426 46.13669294925971 0 280.3378758098314 58.59029226518994 -0.02521528431241333 relativeToGround #msn_ylw-pushpin_copy:0_copy7511000 -80.99354018030583,46.13652675888388,0 G76 53 a-c (TS G1-48 7592), undeformed Sudbury Diabase - 520585 , 5139025 0 North side of road to Red Deer Lake; outcrop east of the road junction; samples a,b,c, are coarse, medium, and fine, respect.; dike trends 210, uncorrected declin=9, and is cut by vein of pegmatite adjacent to which the margins of the mafic dike seem to be fine grained; well preserved ophitic texture; olivine preserved in some large cpx plates; some cpx plates are totally recrystallized to granular aggregates of light green almost colourless amphibole?; well developed corona garnet often symplectic -80.73374442062645 46.40708183090373 0 4067.435779413344 0 0.09034506063707333 relativeToGround #msn_ylw-pushpin_copy:0_copy8410100 -80.73220740851977,46.40450010199757,0 Agmatite - 520589, 5138949 0 -80.73286247953823 46.40354217142856 0 429.8659564582081 0 0.09098515900495909 relativeToGround #msn_ylw-pushpin_copy:0_copy303001 -80.7321935008531,46.40372977691289,0 Gabbro and dikes 0 -80.73286247953821 46.40354217142856 0 3704.119884449832 5.167970385246078e-012 0.09098515900495328 relativeToGround #msn_ylw-pushpin500021 -80.73503248104332,46.40949433708934,0 Burwash-Killarney Rd jnct 0 1 Burwash 0 -80.8117684245988 46.26483653618375 0 2962.81406594571 4.947558958362154e-012 -0.000496724879037525 #default_copy:0_copy710000100110 -80.81379479213497,46.26349830780083,0 G75 4a (TS p1-88) garn.-cpx rock =Sudbury diabase, with plag. xenocrysts; G75 4b amphibolite margins; also KR78 1 (TS G1-77); G7531 marginal s 0 Garnet granulite; east side of highway 69, 1.5 miles north from junction with Killarney Road; sample oriented 211, 250; diabase almost totally recrystallised; only relict mineral are cloudy and sometimes sagenitic cpx, and flexed laths of clear plagioclase; green amphibole is also now evident as coronas; garnet and cpx have been analyzed by Harvey; photos May75T3 30-33; 30 shows baked margin in the gneiss and euhedral megacrysts of plag.; 32 shows deformed part of the contact; 33 shows east intrusive margin and north tectonic? margin; 33 close up of 32; Outcrop http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/suddiabwplagmegacm.jpg http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Photos/suddiabcntctBurwashm.jpg -80.80133844528258 46.24081251250513 0 812.4760436809532 38.2494175284202 0.0004083318275836554 relativeToGround #sn_ylw-pushpin_copy211201001 -80.80156445288652,46.23986086843813,0 G75 5, G75 32a (G1-43) Deformed Sudbury diabase + plag. xenoc. 0 Garnet granulite/amphibolite outcrop east side of Highway 69 1.7 miles south of the Killarney Road junction; one one end of the specimen can be seen a large plag phenocryst with a garnet rim; -80.77287890056945 46.22424963499901 0 1149.060898269446 2.139506688872385e-013 0.1341967059757162 relativeToGround #sn_ylw-pushpin_copy:0_copy870012 -80.77159931968888,46.22365393833414,0 Sudbury diabase, deformed but with plag xenocrysts (not sampled) 0 -80.77515026345576 46.21199664762587 0 169.8000570627856 1.447834306994558e-012 0.1325567781080378 relativeToGround #sn_ylw-pushpin_copy:0_copy88060 -80.77550929238151,46.21211825367885,0 Trout Lake 0 Maps 0 Trout Lake 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Grenville_Front/Grenville_maps/Lumbers_Trout_Lake.jpg 0.75 46.30427814516322 45.99651490098824 -80.48466067803372 -80.80071725331931 Trout Lake 0 -80.6286777055517 46.22282997475276 0 3977.761963679728 0 0.2275773054271386 relativeToGround #msn_ylw-pushpin_copy:0_copy310101010 -80.6194850106954,46.22600387877936,0 Sudbury diabase cont. G76 56 0 -80.6597191726519 46.22359747610464 0 1855.862212375924 3.331012581821555e-011 0.1730033240279453 relativeToGround #msn_ylw-pushpin_copy:0_copy48000120 -80.66330937712274,46.22905416136753,0 ?G76 55 (TS G1-50 7594) calc-silicate? 0 -80.6392536329144 46.22583448844418 0 1855.862212375924 4.423185072413008e-011 0.1877807121670203 relativeToGround #msn_ylw-pushpin_copy:0_copy831010 -80.64496835673924,46.22673325188761,0 ?G76 54 (TS P1- 94 123 7593a); amphib w. cpx venlets & patches cpx-grnt 0 -80.63552980320657 46.23030724870672 0 1855.862212375924 3.331012581822313e-011 0.1904687241787648 relativeToGround #msn_ylw-pushpin_copy:0_copy80010 -80.63462074960992,46.22963766436643,0 ?G76 56 a-c (TS G1-45 7590a, 46 7590b, P1-122); Sudbury diabase a-coarse; b,c fgrain WSW margin 0 NNW trending garnet rich diabase dike, north shore of small island on south shore of Trout Lake; diabase is present on both shores of Trout Lake but not shown on the north shore on the Burwash sheet;strongly recrystallized but some relict plates of dusty oxide filled cpx; cpx recrystallises to granular aggregates of light green cpx; green amphibole also present as well as the ubiqutious biotite; some aggregates seem to have a pinkish colour and may be opx after olivine??; note that both the cloudy and clear parts of a deformed plagioclase exhibit strain effects, bent twin planes and fractured grains; many polygonal grains may however have triple junctions, and are unstrained; garnets are also not even slightly disrupted -80.6597191726519 46.22359747610464 0 1855.862212375924 3.331012581821555e-011 0.1730033240279453 relativeToGround #msn_ylw-pushpin_copy:0_copy:0_copy330 -80.66203010005958,46.22465812901666,0 Alban 0 -80.57396313317005 46.10056621304697 0 4726.503986696454 0 -4.905762362629782 #default_copy:0_copy76000101001 -80.57462990225889,46.10012646179678,0 G75 9 quartzite w. magnetite 0 -80.56036681298529 46.10617295312914 0 1892.985667985195 0 0.2875968502343592 relativeToGround #sn_ylw-pushpin_copy:0_copy3310000010 -80.56318964494415,46.10592278219324,0 Turn off 64 onto 637 to Kilarney 0 -80.77660671816811 46.22673424721873 0 726.0947504721602 0 -5.051686030098946 #default_copy:0_copy7501101100 -80.77595748933703,46.22752412639611,0 Naiscoot Lake diabase 0 -80.39398496761275 45.64501503605897 0 2514.068640192582 0 -4.77243807981149 #default_copy:0_copy7700020200 -80.40012462795919,45.64885530231556,0 Pointe au Baril 0 -80.37386226944317 45.6016411852151 0 3121.204734372006 0 -4.763025201482964 #default_copy:0_copy7802010041 -80.37753671731809,45.60094085483615,0 Shawanaga metagabbro 0 -80.25937241233476 45.54017527735007 0 2141.212217243723 0 -4.676312949082027 #default_copy:0_copy7900000000 -80.26752777777777,45.53997222222223,0 Nobel stop 1 eclogite 0 -80.10516618081647 45.42317515323413 0 108.9998002134878 0 -0.2330014752822466 relativeToGround #sn_ylw-pushpin_copy:0_copy60320 -80.1052890991165,45.42300587042391,0 Nobel - Tim's Horton 0 -80.06170460050302 45.40080178320429 0 2188.172420561606 0 -4.535414678729664 #default_copy:0_copy8100121000 -80.06493327986746,45.40249378887701,0 Parry Sound stop 2 0 -80.01228755199422 45.36704537140346 0 4593.626141207202 0 -4.500240246039957 #default_copy:0_copy820000103 -80.03331295243045,45.36017354346964,0 Parry Sound stop 1 0 -80.01228755199422 45.36704537140346 0 4593.626141207202 0 -4.500240246039957 #default_copy:0_copy8300000102000020 -80.02189562890673,45.36491969798337,0 Parry Sound 0 -80.03286694920129 45.34343800356662 0 3159.271628336584 2.635810748349923e-011 -4.515031088337079 #default_copy:0_copy840002000300 -80.03129110048006,45.34152356464691,0 Gibson Lake Marble 0 -79.77740639278815 44.95126137046437 0 606.8370678193613 0 -4.334095462489813 #default_copy:0_copy85+nicon=http://maps.google.com/mapfiles/kml/pal3/icon63.png+hicon=http://maps.google.com/mapfiles/kml/pal3/icon55.png022100 -79.77757747676499,44.95099540075346,0 Barrie - FutureShop 0 -79.70282920013352 44.40545393457595 0 1122.14024376253 0 -4.270670943250626 #default_copy:0_copy85+nicon=http://maps.google.com/mapfiles/kml/pal3/icon63.png+hicon=http://maps.google.com/mapfiles/kml/pal3/icon55.png022100 -79.70300642185791,44.40620037556914,0 Callender 0 Callander Bay 0 -79.39296350124376 46.20849816972895 0 7067.292701706044 5.835255037128314e-012 -2.379155333488445 #default_copy:0_copy58+nicon=http://maps.google.com/mapfiles/kml/pal3/icon63.png+hicon=http://maps.google.com/mapfiles/kml/pal3/icon55.png00311 -79.38690165032406,46.21404186940762,0 Maps 0 Callander 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Callander/Callander.jpg 0.75 46.24070470988462 46.18876178966484 -79.34401773513476 -79.43448619472295 -1.593367980643437 Grenville 0 Percy Lake 0 -78.36010096842382 45.22166549323155 0 4707.536966674033 0 0.3801657582143884 relativeToGround #msn_donut_copy491 -78.35621430470282,45.22342183955739,0 Tory Hill 0 -78.27077242849867 44.97982504395796 0 23991.68821817088 0 0.442766243410752 relativeToGround #msn_donut_copy5210 -78.27573185621748,44.97284947786434,0 Carnarvon 0 -78.69542540161368 45.0450912929542 0 5499.223443702007 0 0.1424203793953821 relativeToGround #msn_donut_copy470 -78.6980765265767,45.04541900994947,0 Minden 0 -78.71955937777985 44.92369414058234 0 7054.477436771287 0 0.1189174731828138 relativeToGround #msn_donut_copy48011 -78.72407516179179,44.92478576779123,0 Peterborough 0 -78.28386474263463 44.29842714257907 0 11247.51037929639 0 0.4276248301920832 relativeToGround #msn_donut_copy45 -78.28226559697941,44.29392388123538,0 Dorset 0 -78.89316203296471 45.24463719980408 0 1279.238485675943 0 0.002044938833814881 relativeToGround #msn_donut_copy461 -78.89545473461,45.24466237873458,0 Cardiff 0 -78.0127875015249 44.99802225764023 0 997.3188616399468 9.944308909024033e-012 0.001323999184150072 relativeToGround #msn_donut_copy432001 -78.0135059898676,44.99941465480294,0 Bancroft 0 -77.85299888623629 45.0560507600714 0 1293.704038892629 0 -3.946955963039003e-007 #msn_donut_copy44011 -77.85299888623629,45.0560507600714,0 Haliburton 0 -78.50520033861288 45.04553783674525 0 3211.005866753628 0 -0.01720974205258952 relativeToGround #msn_donut_copy41111 -78.514404341448,45.04686126422621,0 Marmora Iron Mine 0 -77.66647200511045 44.48240404228813 0 20200.38051221528 3.565936092466293e-011 2.324321642343507 relativeToGround #msn_donut_copy421011 -77.6581166380291,44.47826094670063,0 Princess Mine 0 -77.78425331672986 45.05854651684939 0 5825.840542213919 0 -0.0003825304483100194 relativeToGround #msn_ylw-pushpin03 -77.78380956981421,45.06720601643899,0 Quadraville Beryl Pit 0 -77.3494519799679 45.30217895175618 0 31011.4159933466 0 0.1245165933917549 relativeToGround #msn_ylw-pushpin16 -77.37795666153869,45.31428430470901,0 Egan Chutes 0 -77.72948886594088 45.07045053886829 0 5279.550433584494 0 -0.008010628641709872 relativeToGround #msn_ylw-pushpin2 -77.73503525428686,45.07499946208894,0 Cardiff Mine dump 0 -78.02996295159421 44.99265373322842 0 3905.523180552725 0 0.4455851280799414 relativeToGround #msn_ylw-pushpin11 -78.03297191445833,44.9929400613969,0 Hway 118/121 0 -78.24833283746338 44.97978184969426 0 2797.633124032087 0 0.02147193141603361 relativeToGround #msn_ylw-pushpin17 -78.24908128802561,44.97851051563991,0 gabbro-dikes ??? 0 -78.24833283746338 44.97978184969426 0 2797.633124032087 0 0.02147193141603361 relativeToGround #msn_ylw-pushpin27 -78.23596307607046,44.98253465890935,0 Gabbro-dikes 0 -78.25886153481899 44.97447415079023 0 2797.633124031395 0 0.01402959691853861 relativeToGround #msn_ylw-pushpin4 -78.26231217309579,44.97588864084343,0 Essonville 0 -78.30264801048766 45.00564262454527 0 2797.633124033183 0 -0.01692190292650826 relativeToGround #msn_ylw-pushpin26 -78.30500699356965,45.00453333269506,0 Bear Lake Diggings 0 -78.32998428102995 44.96155349018194 0 1350.915433828173 0 0.01403001083567169 relativeToGround #msn_ylw-pushpin22 -78.3289709135326,44.96114561828899,0 Warwickite 0 References: - Geological Survey of Canada Miscellaneous Report 39. - Sabina, A.P. (1982): Some rare minerals of the Bancroft area. Mineralogical Record 13 (4), 226]]> -77.98636360819063 45.09298860756147 0 8369.061980988323 0 -0.007573564757352849 relativeToGround #msn_ylw-pushpin24 -78.01575762363368,45.08595236666702,0 Greenmantle Farm 0 http://www.youtube.com/watch?v=h-wBaDVrDIE&feature=geosearch -78.26385500000001 45.00996400000002 0 17493.15789675197 0 7.951386703658792e-015 relativeToGround #msn_ylw-pushpin1 -78.2395601666818,45.01753061117496,0 Highway 62 0 -77.83687117719376 45.04787835285055 0 9035.97060529848 0 0.4385889683556779 relativeToGround #msn_ylw-pushpin18 -77.83328953072261,45.04368621753849,0 Faraday Hill 0 -78.00210573470386 45.00285101911843 0 3956.951002018647 0 -0.2524234148047231 relativeToGround #msn_ylw-pushpin0 -78.00475863497132,45.00406567780856,0 Coe Hill Gold 0 -77.89215568435006 44.93570888840357 0 32663.58793078602 0 -0.1747321744286556 relativeToGround #msn_ylw-pushpin15 -77.89612449399866,44.9225171733552,0 Wilberforce 0 -78.22142819101268 45.03535980450683 0 2056.330810997606 0 0.0009132796738738464 relativeToGround #msn_ylw-pushpin23 -78.22276132326459,45.03684770655397,0 Monck Road 0 -77.99759700642009 45.00872892431183 0 3094.728625857762 0 0.1591150513130356 relativeToGround #msn_ylw-pushpin19 -77.99452408708558,45.01301009110684,0 Silver Crater Mine 0 -77.99759700642009 45.00872892431183 0 3094.728625857762 0 0.1591150513130356 relativeToGround #msn_ylw-pushpin21 -78.009044763765,45.01193536646764,0 Desmont Mine? 0 http://www.couplesresort.ca/Attractions/mines.html -78.22208407874588 45.03690007889672 0 10763.56520645058 0 0.0004494663674177683 relativeToGround #msn_ylw-pushpin3 -78.21300174875476,45.03380787316718,0 Bancroft Motor Inn 0 -77.86224685283733 45.08471652185042 0 413.7918993171211 0 0.00340783925125188 relativeToGround #msn_ylw-pushpin6 -77.86278811910735,45.0845254649807,0 Highway 28 0 -77.88856481635622 45.04057151744632 0 12068.3023452078 0 -0.01521760438715414 relativeToGround #msn_ylw-pushpin13 -77.91190024134785,45.02068581886895,0 Highway 32 0 -78.27093679455413 44.38716734750076 0 123565.9305740293 0 -0.2811754372027951 relativeToGround #msn_ylw-pushpin14 -78.27093679455413,44.38716734750076,0 Portneuf, Shawinigan, Quebec 0 Shawinigan 0 -72.72210368509074 46.56081142289543 0 33221.94391032401 0 0.02490503023013073 relativeToGround #msn_ylw-pushpin1003 -72.7387584060964,46.55874425532158,0 La Tuque 0 -72.74456085400441 47.45415948628785 0 33221.94391032542 0 0.009068686535967596 relativeToGround #msn_ylw-pushpin_copy125000010 -72.77734591359251,47.44307256438455,0 Portneuf-topo_stops 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf8.jpg 0.75 46.93727704332801 46.49634668833403 -72.4967884544071 -73.00809579126729 0.5449203360289923 Maps - geology 0 Structural elements 0 3 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf4.jpg 0.75 47.0747169536238 45.83442574267764 -71.33639246122272 -74.02898097551599 0.04835587836394571 Portneuf Geology Fig 2 0 Map Legend http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf2lgnd.jpg 1 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf2.jpg 0.75 47.85817140133612 46.47838970412991 -71.73512515952918 -73.26527954481036 Portneuf - Geology, Fig 3, showing excursion stops 0 Field Guide http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf_guide.rtf ********** Stop1 Pelitic rocks of the Saint Boniface paragneiss sequence 670200E ; 5157200N Sillimanite-gamet porphyroblastic pelitic gneiss. Paragneiss is severely sheared and migmatitic. The rocks are cross-cutted by a number of ductile and ductile-brittle shear zones, and by minor normal faults. Note the presence of a few thin diabase sheets along post-Grenvillian faults. ********** Stop 2. Quartzite layers of the Saint-Boniface paragneiss sequence 669800E ; 5157175N Typical impure quartzite layer of the Saint-Boniface paragneiss sequence. Such quartzite layers are commonly decimetre to metre thick; they are discontinuous and rarely outcrop as mappable rock unit. ********** Stop 3. Anatexis of the Saint-Boniface paragneiss sequence 667250E ; 5153550N Highly sheared calc-silicate gneiss and migmatitic metapelite hosting slightly discordant sheets oftourmaline-gamet bearing leucogranite and variably boudinaged and desaggregated pegmatite dykes. ********** Stop 4. Intrusive and structural relationships between the Saint-Didace Monzonite and the Shawinigan Gabbronorite 661050E ; 5156250N The Saint-Didace Monzonite is the largest late-Grenvillian granitoid intrusive in the region. This is a composite body dominated by porphyritic monzonite and granite. Although largely massive, the rocks commonly grade to gneissic, and more locally to mylonitic namely at proximity to lithological contacts. A massive porphyritic monzonite sample has yielded a zircon crystallization age at 1072 +/- 2 Ma (unpublished). The granitoid rocks of the Saint-Didace Monzonite are associated with small gabbroic bodies including the Shawinigan Gabbronorite. The latter has yielded a zircon igneous crystallisation age ca. 1077 +10/-2 Ma (Corrigan and van Breemen, 1997). This set of outcrops to be visited features intrusive and structural relationships between granitoid rocks and gabbronorite suggesting magma mixing and syntectonic emplacement. ********** Stop 5. Tectonic contact, via a mylonitic granite sheet, between the Shawinigan Gabbronorite and the Saint-Boniface paragneiss 664050E ; 5155350N The contact zone corresponds commonly to a mylonitic granite sheet. Note that the structural overprint in the paragneiss is indicative of intense, although heterogeneous, ductile deformation. Is the anatexis of the paragneiss contemporaneous with the syntectonic emplacement of the gabbronorite? ********** Stop 6. 'Old grey tonalitic orthogneiss' of the Shawinigan region 671400E ; 5158400N Such polydeformed migmatitic orthogneisses of the Jesuite complex are fairly common in the Shawinigan region. Are these rocks correlative with tonalitic orthogneisses of La Bostonnais Complex, of the Adirondacks Highlands,...? ********** Stop 7. Late-Grenvillian ductile-brittle extensional shear zones 672375E ; 5159750N Gneisses of the eastern strand ofMorin Terrane are cut by late-Grenvillian ductile-brittle shear zones commonly hosting sheared and boudinaged pegmatite. These shear zones occur in conjugate sets, each shear zone with modest displacement. This shearing is attributed to penetrative gravitational collapse following crustal thickening and peak grenvillian regional metamorphism. ********** Stop 8. Recumbent folds developed in mylonitic augen granite, lower part of the Jesuite complex 675025E ; 5163050N llustrates the most common type of folds present in the Jesuite complex. Folds are developed in mylonitic, initially K-feldspar porphyritic monzogranitic orthogneiss. ********** Stop 9. Distributed conjugate extensional shears in retrogressed granulite. ********** Stop 10. Interleafed metagabbro and K-feldspar porphyritic monzogranitic orthogneiss of the structurally lower part of the Jesuite complex 675150E ; 5166500N Gabbroic rocks are lithologically varied, including coarse-grained anorthositic-gabbro. Strain varies widely across the outcrop with marked gradients along lithological contacts. Are the contact relationships intrusive or structural? ********** Stop 11. Transposed and boudinaged mafic dykes in Mekinac-Taureau charnockitic orthogneiss ********** Stop 12. Marble tectonic injections in Mekinac-Taureau charnockitic orthogneiss. ********** Stop; 13. Ductile shear zones and marble tectonic breccia; Mekinac-Taureau domain 671450E;5176000N Mekinac-Taureau domain orthogneisses are interrupted by dispersed paragneiss screens including structurally concordant sheets of marble tectonic breccia. These rocks contain abundant features resulting from intense ductile flow including sheetfolds. Marble tectonic breccia typically outcrops as metre-thick sheets spread over ten s to a few hundreds of meters along strike. They commonly intervene between contrasting rock types. Such tectonic marble breccia sheets are viewed as marking ductile fault zones, although the magnitude of tectonic transport is unknown. ********** Stop 14. Metaplutonic make up of Mekinac-Taureau domain 674900E ; 5172625N This outcrop area allows for a close examination of the various granulite facies metaplutonic rock types which make up much of the Mekinac-Taureau domain. These are generally of monotonous appearance, although displaying a number of distinctive lithological attributes indicatives of a complex intrusive and metamorphic heritage Are all these rocks resulting from a single plutonic event? Which textural / structural overprinting features can be attributed a plutonic vs. metamorphic origin? What are the diagnostic evidences for poly-phased regional deformation and metamorphism? ********** Stop 15. Tectonic boundary between Mekinac -Taureau domain and Morin terrane 677775E ; 5177000N The high-grade orthogneiss at this locality is part of the Mekinac-Taureau domain footwall beneath Monn Terrane Deformation and metamorphic structures are indicative of intense ductile deformation at or near peak metamorphic conditions. Boudinaged and dispersed mafic boudins provide a qualitative stain marker. Note the abundance of granitic mobilisate in the felsic rocks and the presence of orthopyroxene in amphibolite. 2 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf3.jpg 0.75 47.2549530106736 46.48793679368735 -71.96330729288174 -73.03446204085589 -0.4210125135940422 Maps - magnetic 0 Magnetic anomaly map Fig 5 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf5.jpg 0.75 47.88850347502783 46.36090274570205 -71.36917876450491 -73.33970588041635 Magnetic anomaly map Fig 6 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf6.jpg 0.75 47.86173377118586 46.3820346119929 -71.43549704636433 -73.28957106855502 1st vertical derivative map of the residual magnetic field Fig 7 0 http://instruct.uwo.ca/earth-sci/fieldlog/Grenville/Portneuf/portneuf7.jpg 0.75 47.86051311047406 46.47532498320636 -71.46594446060809 -73.27978486101701