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Carube Copper Corp.
Summary
| Project: | Bellas Gate | |
|---|---|---|
| Deposit: | Bellas Gate | |
| Location: | Jamaica | |
| Commodities: | Copper-Gold | |
| Date: | 7/5/2017 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 5-7-2017: Carube Copper Corp. announces an Exploration/Drilling Update report for its Bellas Gate deposit at the Bellas Gate project. Drilling results incl. 340.10m @ 0.09ppm Au, 0.20% Cu from 45.30m. Ottawa, Ontario--(Newsfile Corp. - July 5, 2017) - Car | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Shannon Baird (Internal) | |
| ABSTRACT: | Ottawa, Ontario--(Newsfile Corp. - July 5, 2017) - Carube Copper Corp. (TSXV: CUC) is pleased to report the results from PVT-17-004, the initial hole drilled in a 2,000m program within the 100% owned Bellas Gate Project in Jamaica. Jeff Ackert, President and CEO of Carube Copper commented, "The wide intersection of continuous mineralization and alteration in this drill hole, along with the evidence from surface exploration, confirms that the Provost Prospect represents a genuine copper-gold porphyry. The higher-grade zone in PVT-17-004 seems to be similar to the zone intersected in Hole PVT- 16-002 and could represent peripheral veining and overprinting in the upper portions of the copper porphyry system." A second hole has been completed at Provost, which also intersected copper mineralization; assay results are pending. Further drilling is anticipated once the results from the second hole have been received. Drilling is presently on-going at the Provost SE Prospect, one of the five high priority targets scheduled for drilling in 2017. PVT-17-004 was drilled to expand a zone of newly discovered mineralization that was drilled in 2016. It targeted a zone beneath a significant copper-gold soil anomaly that is also coincident with a favourable porphyry "signature" combining geology, alteration, soil geochemistry, and geophysics. The hole encountered mostly volcanic andesite along with several narrow monzonite to hornblende porphyritic dykes throughout, ranging in age from pre-mineral to post-mineral. Chlorite-sericite alteration was encountered briefly at the beginning of the hole but graded into potassic alteration comprised of k-feldspar, magnetite and biotite, which continued until the end of hole. | |
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