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Project: | Qembo Dome | |
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Deposit: | Qembo Dome | |
Location: | Namibia | |
Commodities: | Copper-Silver | |
Date: | 11/18/2019 | |
Report Code: | JORC | |
Report Type: | Exploration/Drilling Update | |
Project Stage: | Pursuing Resources Definition | |
Report details: | 18-11-2019: Kopore Metals ltd. announces an Exploration/Drilling Update report for its Qembo Dome deposit at the Qembo Dome project. Drilling results incl. 2.07m @ 0.5% Cu, 65.96g/t Ag from 129.67m. Kopore Metals Limited (Kopore or the Company) is pleased | |
Resources: | x | |
CP/QP: | [Overall Report]: David Catterall (Internal) | |
ABSTRACT: | Kopore Metals Limited (Kopore or the Company) is pleased to report its first copper mineralisation assay results on the Qembo Dome Prospect, on the Kalahari Copper Belt in Namibia. The intercept, in diamond drill hole QBDD001 is at 117m below surface. The Otjari/Qembo corridor extends laterally from the SW to NE a distance of 113km and contains the interpreted subsurface Otjari Domal Prospect (estimated strike length around the dome of 94km) and the identified Qembo Dome Prospect (estimated strike length around the dome of 96km). Kopore’s exploration has recently focussed on the Otjari/Qembo corridor as a high priority target area as it continues in its quest to find the next copper deposit on the Kalahari Copper Belt. The Qembo geological model has been interpreted as comparable to domes located in the north-west of the Kalahari Copper Belt in Botswana. Most significantly, this region includes the Zone 5 mine currently under construction by US private company, Cupric Canyon (approximately 275km from Qembo) while the Otjari Dome Prospect has similar interpreted characteristics to Sandfire Resources’ (ASX:SFR) T3 Deposit (approximately 165km from Qembo). The mineralised intersection in QBDD001 has been interpreted as located on the targeted D’Kar/Ngwako Pan Formation geological contact position, known to host copper mineralisation across the Kalahari Copper Belt. Identified visible copper minerals include chalcocite, trace amounts of bornite, malachite and chrysocolla. The oxidised mineralisation is located 34m below the base of the Kalahari sand and calcrete horizon. The intersection of visible copper mineralisation confirms a previously reported reverse circulation (RC) historical mineralised intersection (3m @ 1.11% copper1 ). | |
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