000	00000nam 2200000zi 4500
001	9.956304
003	CaOODSP
005	20251031142449
006	m     o  d f
007	cr |n|||||||||
008	251014t20132013oncdab  ob   f|0| 0 eng d
040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn-mb
086	1 |aM183-2/7372E-PDF
100	1 |aCaté, A, |eauthor.
245	10|aPreliminary observations on the geological environment of the Paleoproterozoic auriferous volcanogenic massive sulphide deposit of Lalor, Snow Lake, Manitoba / |cA. Caté, P. Mercier-Langevin, P.-S. Ross, S. Duff, M. Hannington, B. Dubé, and S. Gagné.
264	1|a[Ottawa] : |bGeological Survey of Canada, |c2013.
264	4|c©2013
300	|a1 online resource (13 pages) : |bcharts, illustrations, maps.
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aOpen file, |x2816-7155 ; |v7372
504	|aIncludes bibliographical references (page 13).
520	|a"The Lalor auriferous VMS deposit in the Proterozoic Flin Flon‐Snow Lake belt of Manitoba is a recent deep (>500 m) discovery by HudBay Minerals that is currently being developed for commercial production. It contains approximately 27 Mt of ore potentially including 75 t of Au as well as 684 t of Ag, 1.38 Mt of Zn and 0.2 Mt of Cu. This deposit is an ideal “natural laboratory” to better understand the signature and key characteristics of auriferous VMS deposits and elucidate characteristics that can be used to vector toward them (Mercier‐Langevin et al., 2012). The deposit is situated in the Flin Flon greenstone belt which is part of the Paleoproterozoic Trans‐Hudson orogen. Lalor has been affected by several hydrothermal events, an intense polyphase deformation and an amphibolite grade metamorphism"--page 3.
650	0|aSulfide minerals|zManitoba|zSnow Lake.
650	6|aSulfures (Minéralogie)|zManitoba|zSnow Lake.
710	2 |aGeological Survey of Canada, |eissuing body.
830	#0|aOpen file (Geological Survey of Canada)|v7372.|w(CaOODSP)9.506878
856	40|qPDF|s2.04 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m183-2/M183-2-7372-eng.pdf