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Rockcliff Copper Corp.
Summary
| Project: | Talbot | |
|---|---|---|
| Deposit: | Talbot | |
| Location: | Canada | |
| Commodities: | Gold | |
| Date: | 11/1/2016 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resource Increase/Upgrade | |
| Report details: | 1-11-2016: Rockcliff Copper Corp. announces an Exploration/Drilling Update report for its Talbot deposit at the Talbot project. JV with Hudbay Minerals Inc. - drilling results incl. 6.27m @ 9.0% CuEq from 713.2m. Toronto, ON – November 1, 2016 – Rockcliff | |
| Resources: | (Resource, Inf.): 2.168Mt @ 2.8% Cu, 2.4g/t Au, 2.2% Zn, 54.6g/t Ag | |
| CP/QP: | [Overall Report]: Ken Lapierre (Internal) | |
| ABSTRACT: | Toronto, ON – November 1, 2016 – Rockcliff Copper Corporation (“Rockcliff “or the “Company”) (TSX.V: RCU) is pleased to announce the first drill hole assay results from its phase 2 drill program on the Talbot Property, Manitoba. Drill hole TB-011 intersected multiple lenses of volcanogenic massive sulphide (VMS) mineralization with the following composite results. Ken Lapierre, President and CEO commented, “With high grade copper and gold assays in multiple zones including a newly intersected mineralized hangingwall zone, we have decided to increase our planned drill meterage to 6,000 metres from its original 5,000 metres. All three lenses have significant grades while the main lens contains high grade gold mineralization which could have significant economic benefits for the property moving forward. The gold-rich Talbot copper deposit is open in all directions and we look forward to expanding its limits as well as testing proximal high priority geophysical targets.” TB-011 was drilled at UTM NAD83 co-ordinates 458451E/5997044N, to a depth of 785 metres, along an azimuth of 285 degrees, and a dip of -70 degrees. The gold-rich Talbot copper deposit is defined as a stratabound, VMS deposit consisting of several lenses of coarse grained to stringer to massive sulphides of pyrite, chalcopyrite, sphalerite and pyrrhotite in a quartzofeldspathic gneiss. The depositional environment is similar to that of present and past producing base metal deposits of bi-modal volcaniclastic rocks in the Flin Flon – Snow Lake Greenstone Belt. | |
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