Wellgreen Platinum Ltd.
  • Home
  • About us
    • Profile
    • Management
    • Board of Directors
    • Governance
    • Social Responsibility
  • Projects
    • Wellgreen ›
      • Overview
      • 2015 PEA
      • 2014 Resource Estimate
      • Location & Geology
      • Image Galleries
    • Other Projects ›
      • Shakespeare
      • Fox Mountain
      • Shining Tree
  • Investors
    • Corporate Presentation
    • Upcoming Conferences
    • Share Structure
    • Analyst Coverage
    • Financial Reports
    • Filings
    • News Releases
      • 2015
      • 2014
      • 2013
      • Archives
      • Technical Releases
  • Contact
    • Contact Us
    • Careers
Projects
  • Wellgreen
    • Overview
    • 2015 PEA
    • 2014 Resource Estimate
    • Location & Geology
    • Image Galleries
  • Other Projects
    • Shakespeare
      • Overview
      • Location & Geology
      • Image Galleries
    • Fox Mountain
    • Shining Tree

INVESTORKIT

  • March 2015 - Corporate Presentation
  • Wellgreen 2015 PEA Technical Report
  • Wellgreen 2014 Mineral Resource Technical Report

STOCKINFO

Mar 18, 2015 12:55 AM EST
WG 0.52 +0.02
WGPLF 0.421 +0.011

RECEIVE THE LATEST NEWS RIGHT TO YOUR EMAIL

Fox Mountain

Print Friendly Version of this pagePrint Get a PDF version of this webpagePDF

Wellgreen Platinum’s 100%-owned Fox Mountain property is located approximately 50 kilometres north of Thunder Bay, within the Mid-Continent rift of Northwestern Ontario and consists of 14 unpatented claims covering approximately 3,312 hectares. The Fox Mountain intrusions are interpreted to be fault controlled and are related to Mid-Continent rift magmatism.

Airborne magnetic and EM surveys were conducted on the Fox Mountain property in November 2010 and followed up by drilling of two holes totaling 513 metres, in early 2011. This early exploration identified a sub-horizontal 4-5 metre thick layer of massive magnetite-iron sulphide skarn mineralization within the Sibley Group sedimentary rocks. Both holes intersected massive magnetite with pyrite, pyrrhotite, and chalcopyrite mineralization within sub-horizontally bedded Sibley Group mudstones that are intruded by diabase and olivine gabbro. Hole U17-01 intersected 5.45 meters grading 46.1% iron, 0.073% cobalt and 0.12% copper and hole U17-02 intersected 4.31 meters of 31.9% iron with 0.071% cobalt and 0.14% copper. The skarn-type mineralization is thought to be the result of replacement of carbonate rich sedimentary rocks by metal-rich fluids related to gabbro intrusions.

 

 

Click here for the Qualified Person information, Legal Notice, forward-looking information and the cautionary note.

Wellgreen Platinum Ltd.
  • About us
  • Projects
  • Investors
  • Contact
  • Legal
  • Privacy
  • Sitemap
  • Toll Free Telephone +1.888.715.7528
  • 420-1090 West Georgia Street

    Vancouver, BC Canada V6E 3V7

  • Email:[email protected] Download vCard

© Copyright 2015 Wellgreen Platinum Ltd. All Rights Reserved

Website Design & Development by: Aroma Web Design