04BHA-0462 Granophyre, Kamiskotia Gabbroic Complex, Robb Township (NAD83, Zone 17 UTM 451049E, 5381502N; #3 on Figure 2 and Table 1) In central Robb Township, a granophyric phase <strong>from</strong> <strong>the</strong> Upper Zone (Barrie 1992) <strong>of</strong> <strong>the</strong> large Kamiskotia Gabbroic Complex (KGC) crops out approximately 1.7 km northwest <strong>of</strong> Kamiskotia Lake. A representative sample collected <strong>from</strong> this locality (04BHA-0462) consists <strong>of</strong> quartz, altered plagioclase, granophyric intergrowth, and minor opaques, chlorite and epidote. Zircon recovery <strong>from</strong> <strong>the</strong> sample was sparse, but an adequate number <strong>of</strong> good quality grains were found for analysis. These comprised colourless to pale pinkbrown irregular grain fragments, parts <strong>of</strong> skeletal grains and rarer faceted crystals showing low-order faces. Conventional isotope dilution U/Pb analyses <strong>of</strong> three abraded single zircons are concordant to slightly discordant (0.2–0.6%) and yield 207 Pb/ 206 Pb ages between 2704 and 2706 Ma (Table A1). Weighting <strong>of</strong> all three analyses yields a mean age <strong>of</strong> 2704.8±1.4 Ma (53% fit, MSWD = 0.64; Figure 3C), which is considered a robust estimate for <strong>the</strong> age <strong>of</strong> crystallization <strong>of</strong> <strong>the</strong> Upper Zone <strong>of</strong> <strong>the</strong> KGC. The 2704.8±1.4 Ma age for <strong>the</strong> KGC Upper Zone granophyre is slightly younger than, but within error <strong>of</strong>, a 2707±2 Ma age determined for a stratigraphically lower, Middle Zone gabbro dated by Barrie and Davis (1990). The granophyre age is also within error <strong>of</strong> a 2703.1±1.2 Ma age for one <strong>of</strong> <strong>the</strong> lowest dated units (03BHA-0047; this study) <strong>of</strong> <strong>the</strong> Kamiskotia Volcanic Complex, which <strong>the</strong> gabbro and granophyre appear to intrude. 03BHA-0382 Rhyolite, Halfmoon Lake, nor<strong>the</strong>astern Robb Township (NAD83, Zone 17 UTM 452485E, 5383020N; #4 on Figure 2 and Table 1) This sample represents a section <strong>of</strong> rhyolite recovered <strong>from</strong> diamond drill hole collared west <strong>of</strong> <strong>the</strong> Kam- Kotia Mine, at <strong>the</strong> Falconbridge Halfmoon Project, approximately 200 m south <strong>of</strong> Halfmoon Lake. Material for U/Pb dating was collected <strong>from</strong> <strong>the</strong> 97–100.5 m section <strong>of</strong> hole R-44-14. The general zircon population <strong>from</strong> this sample comprises poor to moderate quality, short, pale- to medium-brown stubby, <strong>of</strong>ten ragged, prisms. Better quality grains show sharp, prismatic exteriors although many grains are also broken. A selection <strong>of</strong> <strong>the</strong> highest quality, short (2:1 or less) and/or broken, clear and crack-free prisms, essentially devoid <strong>of</strong> inclusions, were chosen for abrasion and analysis. Three single grains yield completely overlapping data, straddling concordia and ranging between 0.2 and 0.4% reversely discordant (Figure 3D; Table A1). These results produce a weighted mean 207 Pb/ 206 Pb age <strong>of</strong> 2700.0±1.1 Ma (40% probability <strong>of</strong> fit; MSWD = 0.9), which is interpreted as <strong>the</strong> primary crystallization age <strong>of</strong> <strong>the</strong> rhyolite. The 2700 Ma age for <strong>the</strong> Halfmoon Lake rhyolite lies within error <strong>of</strong> <strong>the</strong> age <strong>of</strong> felsic volcanic rocks <strong>from</strong> <strong>the</strong> Genex Mine (03BHA-0345) and confirms a Blake River assemblage age for <strong>the</strong> volcanic stratigraphy immediately north and east <strong>of</strong> Kamiskotia Lake. 03BHA-0384 Felsic lapilli tuff, Kam-Kotia Mine, eastern Robb Township (NAD83, Zone 17 UTM 455853E, 5381788N; #5 on Figure 2 and Table 1) This sample <strong>of</strong> felsic lapilli tuff was collected <strong>from</strong> outcrop approximately 500 m sou<strong>the</strong>ast <strong>of</strong> <strong>the</strong> Kam- Kotia Mine in easternmost Robb Township. Zircons recovered <strong>from</strong> this sample comprise fairly clear, colourless to pale brown short and elongate prism populations. Apatite and fluid inclusions are relatively common. Uranium and Pb isotopic data obtained for four single short prisms are all overlapping and concordant and yield an average 207 Pb/ 206 Pb age <strong>of</strong> 2701.1±1.4 Ma (97% probability <strong>of</strong> fit, MSWD = 0.09; Figure 3E; Table A1). This age, interpreted to reflect <strong>the</strong> primary crystallization <strong>of</strong> <strong>the</strong> tuff, is nearly identical to those obtained <strong>from</strong> o<strong>the</strong>r volcanic units between Halfmoon Lake and <strong>the</strong> Genex Mine and appear to corroborate a Blake River assemblage age for this sequence. 112
03BHA-0345 Felsic lapilli tuff, Genex Mine, central Godfrey Township (NAD83, Zone 17 UTM 458483E, 5369414N; #6 on Figure 2 and Table 1) A sample <strong>of</strong> crystal-rich felsic lapilli tuff was collected <strong>from</strong> an outcrop approximately 800 m southsouthwest <strong>of</strong> <strong>the</strong> Genex Mine. This sample yielded an abundant population <strong>of</strong> relatively large, colourless to pale yellow-brown, water-clear, sharply prismatic or euhedral zircon grains. Best quality grains are dominated by short, stubby or equant forms, though subordinate populations having slightly more elongate, or flat, prismatic morphologies are also present. Rod and bubble inclusions are common in many zircons, but were avoided in <strong>the</strong> final grains chosen for analysis. Data for three abraded single-grain fractions <strong>of</strong> colourless to pale yellow, clear, stubby to equant zircons overlap completely, clustering tightly on or slightly above concordia (
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ISBN 0-7794-8652-8 THESE TERMS GOVE
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ONTARIO GEOLOGICAL SURVEY Open File
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Contents Abstract .................
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Appendix 1. Thermal Ionization Mass
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Miscellaneous Release—Data 155 Di
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The Timmins area and Kirkland Lake-
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Overview of Results from the Greens
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3. The geophysical subproject funct
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The following Preliminary Maps have
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Samples with zircons analyzed by SH
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Figure 4. U/Pb concordia plots of T
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Figure 6. U/Pb concordia plot of TI
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Targeting of several of these overg
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Figure 10. U/Pb SHRIMP results from
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In northwest Cleaver Township, a fe
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SHRIMP U/Pb dating was carried out
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Stratigraphic Framework In this sec
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PACAUD ASSEMBLAGE The 2750 to 2735
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The iron formation and chert brecci
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(thickness) of banded iron-poor iro
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clast conglomerates at the top of t
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BLAKE RIVER ASSEMBLAGE Lower Part T
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The Krist formation consists of cal
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Timmins Area In the Timmins area, t
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Kirkland Lake-Larder Lake Area Hyde
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Intrusion Framework The plutonic ro
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The youngest dated synvolcanic mafi
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Albitite dikes are crosscut by gold
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Worming Geophysical Data Treatment
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In Timmins, the first generation of
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Figure 20. Geological sketch map of
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from Halfmoon Lake, only 2 km to th
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The Blake River Group is divided in
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Figure 22. Geological map of Munro
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Mine stratigraphic succession, have
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Figure 24. Geological map of Currie
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Table 5. Simplified classification
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- Page 102 and 103: Table 7. Diagnostic mineral assembl
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- Page 108 and 109: of the inversion product. (Recent a
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- Page 120 and 121: References Ames, D.E., Bleeker, W.,
- Page 122 and 123: Bleeker, W., Parrish, R.R. and Sage
- Page 124 and 125: Galley, A.G., Pilote, P. and Davis,
- Page 126 and 127: Heather, K.B., Percival, J.A., Mose
- Page 128 and 129: Lesher, C.M., 1989. Komatiite-assoc
- Page 130 and 131: Péloquin, A.S., Verpaelst, P., and
- Page 132 and 133: Stern, R.A. 1997. The GSC sensitive
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- Page 136 and 137: THERMAL IONIZATION MASS SPECTROMETR
- Page 140 and 141: contrastingly have been dated near
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