Discovery And General Geology Of The Gold Quarry Deposit, Eureka County, Nevada

Society for Mining, Metallurgy & Exploration
C. E. Ekburg
Organization:
Society for Mining, Metallurgy & Exploration
Pages:
11
File Size:
543 KB
Publication Date:
Jan 1, 1987

Abstract

Gold Quarry is a sediment-hosted, epithermal disseminated gold deposit located along the Carlin Trend. Gold, hosted by allochthonous Ordovician siltstones and cherts, is localized at the intersection of structures sympathetic to the major Good Hope and Gold Quarry faults. The magnitude of Gold Quarry was discovered in 1979 by surface exploration and by percussion holes drilled near the Maggie Creek orebody. Four years of development drilling delineated an open pit mineable gold deposit that contains 130 Mt (144 million st) of ore at an average 1.68 g/t (0.049 oz per st) of gold and includes a high-grade core of 46 Mt (51 million st) that average 2.64 g/t (0.077 oz per st) gold. Milling of the higher-grade portion began in 1985.
Citation

APA: C. E. Ekburg  (1987)  Discovery And General Geology Of The Gold Quarry Deposit, Eureka County, Nevada

MLA: C. E. Ekburg Discovery And General Geology Of The Gold Quarry Deposit, Eureka County, Nevada. Society for Mining, Metallurgy & Exploration, 1987.

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