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| 02184nam 2200397zi 4500 |
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001 | 9.936735 |
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003 | CaOODSP |
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005 | 20241007081458 |
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006 | m o d f |
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007 | cr cn||||||||| |
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008 | 240412t20242024qucbdo ob f000 0 eng d |
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020 | |a9780660713502 |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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043 | |an-cn-qu |
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086 | 1 |aM183-2/9172E-PDF |
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100 | 1 |aHébert, Serge, |eauthor. |
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245 | 10|aArsenopyrite Re-Os age and zircon U-Pb geochronology of gold prospects, Caniapiscau-Koksoak area, northern Labrador Trough, Quebec / |cS.T. Hébert, P. Mercier-Langevin, R.A. Creaser, N. Wodicka, and P.-S. Ross. |
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264 | 1|aOttawa, Ontario : |bGeological Survey of Canada, |c2024. |
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264 | 4|c©2024 |
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300 | |a1 online resource (27 pages) : |bmaps, graphs, photographs. |
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336 | |atext|btxt|2rdacontent |
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337 | |acomputer|bc|2rdamedia |
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338 | |aonline resource|bcr|2rdacarrier |
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490 | 1 |aOpen file, |x2816-7155 ; |v9172 |
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504 | |aIncludes bibliographical references (pages 11-17). |
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520 | 3 |a"The Labrador Trough of northern Quebec is perhaps best known for its giant iron ore deposits, but shows exploration potential for several other deposits types, including orogenic-style gold. In the Caniapiscau-Koksoak area, gold showings are commonly associated with late structural features in mafic to intermediate intrusive rocks and their vicinity, but the timing of mineralization is unclear. In this study, we provide geochronology results on two samples"--Abstract, page 1. |
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650 | 0|aGold ores|xGeology|zQuébec (Province) |
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650 | 0|aZircon|zQuébec (Province)|xAnalysis. |
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650 | 0|aGeological time|zQuébec (Province) |
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650 | 6|aOr|xGisements|xGéologie|zQuébec (Province) |
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650 | 6|aZircon|zQuébec (Province)|xAnalyse. |
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650 | 6|aGéochronologie|zQuébec (Province) |
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710 | 2 |aGeological Survey of Canada, |eissuing body. |
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830 | #0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v9172.|w(CaOODSP)9.506878 |
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856 | 40|qPDF|s13.85 MB|uhttps://publications.gc.ca/collections/collection_2024/rncan-nrcan/m183-2/M183-2-9172-eng.pdf |
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856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/pmt3329 |
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