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Equinox Gold Corp.
Summary
| Project: | Aurizona | |
|---|---|---|
| Deposit: | Genipapo, Micote, Mestre Chico | |
| Location: | Brazil | |
| Commodities: | Gold | |
| Date: | 3/8/2018 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 8-3-2018: Equinox Gold Corp. announces an Exploration/Drilling Update report for its Genipapo, Micote, Mestre Chico deposit at the Aurizona project. Drilling results incl. 21m @ 84.3g/t Au. March 8, 2018 – Vancouver, BC – Equinox Gold Corp. (TSX-V: EQX, O | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Scott Heffernan (Internal) | |
| ABSTRACT: | March 8, 2018 – Vancouver, BC – Equinox Gold Corp. (TSX-V: EQX, OTC: LWLCF) (“Equinox Gold” or “the Company”) is pleased to announce positive drilling results from near-mine exploration at the Company’s 100%-owned Aurizona Gold Mine (“Aurizona”) in Brazil. Broad intervals of economic grade gold mineralization, including ultra high-grade gold values up to 1,005 grams per tonne gold (“g/t Au”), were intersected near surface at the Genipapo, Micote and Mestre Chico targets. The Company tested six nearmine exploration targets with 45 holes totalling 5,500 metres (“m”). “The bulk of recent exploration work at Aurizona has successfully focused on resource growth at the Piaba West target,” said Scott Heffernan, EVP Exploration of Equinox Gold. “Concurrently, near-mine exploration drilling has highlighted three targets east of the Piaba gold deposit with significant near-surface gold mineralization, clearly demonstrating the growth potential at Aurizona.” The Genipapo target, located east and north of the Piaba gold deposit, measures several square kilometres in area and covers numerous NW-SE trending gold-in-soil and geophysical anomalies. Drilling focused on the largest gold-in-soil anomaly, measuring 500 m by 1,000 m, and has now intersected gold mineralization on three distinct structures within a 400 m wide corridor. The NW-SE orientation of these mineralized structures is new and unique to this portion of the Piaba trend. | |
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