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Kintavar Exploration Inc.
Summary
| Project: | Mitchi | |
|---|---|---|
| Deposit: | Sherlock, Watson | |
| Location: | Canada | |
| Commodities: | Copper-Silver | |
| Date: | 1/31/2018 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 31-1-2018: Kintavar Exploration Inc. announces an Exploration/Drilling Update report for its Sherlock, Watson deposit at the Mitchi project. Drilling results incl. 131m @ 0.31% Cu, 2.85g/t Ag from 44m. Montreal, Quebec, January 31, 2018 – Kintavar Explora | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Alain Cayer (Internal) | |
| ABSTRACT: | Montreal, Quebec, January 31, 2018 – Kintavar Exploration Inc. (the “Corporation” or “Kintavar”) (TSX-V: KTR), is pleased to announce the assays of the first 4 drill holes from its 2017-2018 winter drilling program. Twelve diamond drill holes totalling 1,771 m have been realized on the Sherlock and Watson areas. The favourable sedimentary unit has been intersected by 8 diamond drill holes in the Sherlock area starting from surface and covering over 200 m in width, 200 m in length and 175 m in vertical depth and the unit remains open to the East, West and at depth (figure 1). The sedimentary unit is composed of the calcitic marble enriched in phlogopite/biotite which carries the majority of the copper mineralization and the generally less mineralized calc-silicate units mainly composed of diopside, phlogopite/biotite, feldspar and variable amounts of quartz, scapolite and wilsonite. These horizons are deformed and folded and the alternating sequence of marble and calc-silicate units with locally sCopper mineralization observed in the drill holes ranges from trace to 5% in the form of bornite and chalcopyrite with traces of chalcocite. Pyrite has been observed only locally with less than trace and rarely near 1%. Summary of the main intercepts from the first 4 drill holes is presented in the table below. Drill holes MS-17-01 and 02 have intersected a folded calc-silicate unit and have been stopped once they attained their geophysical targets. Drill hole MS-17-03 demonstrated that mineralization extends farther than expected and as a result the extension of MS-17-01 and 02 is planned for the next drilling campaign. ome levels of gneiss, can be well observed in the core ranging from meters to tens of meters. | |
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