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Project: | Duvay-Chenier | |
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Deposit: | Duvay | |
Location: | Canada | |
Commodities: | Gold | |
Date: | 10/17/2017 | |
Report Code: | NI43-101 | |
Report Type: | Exploration/Drilling Update | |
Project Stage: | Pursuing Resources Definition | |
Report details: | 17-10-2017: Tres-Or Resources Ltd. announces an Exploration/Drilling Update report for its Duvay deposit at the Duvay-Chenier project. Drilling results incl. 10m @ 0.66g/t Au from 18m. Vancouver, B.C. – October 16, 2017 - Tres-Or Resources Ltd. (“Tres-Or” | |
Resources: | x | |
CP/QP: | [Overall Report]: Laura Lee Duffett, Harrison Cookenboo (Internal) | |
ABSTRACT: | Vancouver, B.C. – October 16, 2017 - Tres-Or Resources Ltd. (“Tres-Or”) (TSX-V: TRS, OTCPK: TRSFF) is pleased to report the completion of the Phase 1 drill program at the DuvayChenier gold project, located 15 kms northeast of Amos, and 65 kms north of Val-d’Or, Québec. The drill program comprised 20 drill holes totaling 3207 m, and Phase I tested three main target areas. These three target areas are: 1) the northeast shear zone/strong induced polarization (IP) chargeability target; 2) the Duvay Zone Principal, and 3) coincident magnetic/electromagnetic (EM) and structural targets 2 kms northwest of the Zone Principal, near Lake Obalski. The first forty sample results have been returned from the laboratory. These rushed samples cover only the top 46.5 m of the first drill hole (DUV17-01), but already reveal a new zone of significant gold mineralization. Drill hole DUV17-01 tested the strong chargeability anomaly originally identified from the IPower3D survey and coincident with the northeast shear zone at Duvay. This target is approximately 400 m northeast of the Duvay Zone Principal, in an area of relatively sparse historical work. The sample results from DUV17-01 include 10.0 m of gold mineralization at 0.66 g/t Au from 18.0 m to 28.0 m depth, including an enriched interval of 2.55 g/t Au over 2.0 m from 21.0 to 23.0 m (Table 1). This mineralized interval includes a 5.4 m deformed white quartz vein, with zones of substantial sulfide mineralization and black schist. The true thickness of this zone is not yet known. | |
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