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Osisko Metals Inc V.OM

Alternate Symbol(s):  OMZNF

Osisko Metals Incorporated is a Canada-based exploration and development company. The Company is engaged in the exploration and evaluation of base metals properties with a focus on copper and zinc mineral assets located in Canada. The Company’s projects include the Gaspe Copper project, the Pine Point project, and Mount Copper Expansion project. Its Gaspe Copper project is located near Murdochville in the Gaspe peninsula of Quebec including the copper mountain expansion deposit that hosts a NI43-101 inferred resource of 456 Megaton (Mt) grading. The Company’s Pine Point project is located on the south shore of Great Slave Lake in Canada’s Northwest Territories. It is based on current mineral resource estimates, which is an open pit and shallow underground mining and consist of 12.9 Mt grading. Its Mount Copper Expansion project is a copper resource property, which is located in Eastern North America. The Company’s subsidiary is Pine Point Mining Limited.


TSXV:OM - Post by User

Bullboard Posts
Post by Rocket14on Oct 11, 2018 2:10pm
57 Views
Post# 28782792

Positive Govn't Report

Positive Govn't Report
Seems like really good news coming from Geological Survey of Canada research in the region as well. 
This report presents analytical data from sphalerite, galena, chalcopyrite, and arsenopyrite grains recovered during recent surficial sampling programs in the region southwest of the headwaters of the Mackenzie River, Northwest Territories. Many samples were found to contain high numbers of sulphide mineral grains for which there is no known local source. Lead and S isotopic determinations were conducted to evaluate if the sulphide grains could have been transported from the nearest known source, the Pine Point Mississippi Valley-type district, or whether the grains are sourced from yet-to-be-discovered bedrock mineralization. Lead isotopic values from galena grains (207Pb/204Pb = 15.57 to 15.70; 206Pb/204Pb = 18.00 to 18.20) indicate a more radiogenic source than the Pine Point district and are, therefore, likely to have been locally sourced. Sulphur isotopic values from galena grains range from 0 to 27 permille delta-34S, comparable to Pine Point and other Mississippi Valley-type deposits globally, indicating that similar styles of mineralization may occur in the region. Chalcopyrite delta-34S values range from -22 to +28 permille, indicating that the grains are sourced from either sediment-hosted Cu or Manto-style mineralization. Arsenopyrite delta-34S values indicate a sulphur source similar to orogenic gold deposits near Yellowknife, Northwest Territories, and are likely derived from the Canadian Shield, north of the study area.

source:
https://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan/fulle.web&search1=R=311247
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