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Gold Standard Ventures Corp.
Summary
| Project: | Railroad-Pinion | |
|---|---|---|
| Deposit: | Jasperoid Wash | |
| Location: | United States | |
| Commodities: | Gold | |
| Date: | 2/21/2019 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resource Increase/Upgrade | |
| Report details: | 21-2-2019: Gold Standard Ventures Corp. announces an Exploration/Drilling Update report for its Jasperoid Wash deposit at the Railroad-Pinion project. Drilling results incl. 27.7m @ 0.86g/t Au from 56.7m. VANCOUVER, British Columbia, Feb. 21, 2019 -- Gold | |
| Resources: | ||
| CP/QP: | [Overall Report]: Steven Koehler (Internal) | |
| ABSTRACT: | VANCOUVER, British Columbia, Feb. 21, 2019 -- Gold Standard Ventures Corp. (TSX: GSV; NYSE AMERICAN: GSV) (“Gold Standard” or the “Company”) today reported Phase 2 results from 19 reverse-circulation (“RC”) holes and 2 core holes at the Jasperoid Wash Deposit on its 100%-owned/controlled Railroad-Pinion Project in Nevada’s Carlin Trend (refer to Jasperoid Wash plan and section maps at the following link https://goldstandardv.com/lp/jw-feb19-2019-drillmaps/). Jasperoid Wash is located approximately 6 km south of the Pinion Deposit, 7.5 km southwest of the Dark Star Deposit and 4 km southwest of the Dixie Deposit. The Phase 2 Jasperoid Wash drilling program was designed to expand areas of known shallow oxide mineralization; test new targets north and south of the existing drill pattern; and provide additional material for metallurgical testing. Two holes at Jasperoid Wash intersected thick, near-surface oxide gold mineralization hosted in pervasively altered and oxidized Pennsylvanian-Permian (“Penn-Perm”) debris flow conglomerate and calcarenite - - the same host section as the Dark Star and Dixie deposits. RC hole JW18-37 intersected 25.9m of 0.69 g Au/t, including 6.1m of 1.10 g Au/t; and JW18- 30 intersected 27.7m of 0.86 g Au/t, including 12.2m of 1.17 g Au/t. These results continue to support the lateral and strike -continuity of oxide mineralization at Jasperoid Wash and establish the north-striking dike-filled fault corridor as a control on mineralization. | |
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