Discovery and Geology of the Turquoise Ridge Gold Deposit

Society for Mining, Metallurgy & Exploration
E. J. Berentsen
Organization:
Society for Mining, Metallurgy & Exploration
Pages:
5
File Size:
99 KB
Publication Date:
Jan 1, 1996

Abstract

The Turquoise Ridge gold deposit is located near the Getchell Mine, 72 km (42 miles)northeast of Winnemucca, NV (Fig. 1). The deposit is owned by Getchell Gold Corp. The host rocks consist of Ordovician and Cambrian age shales and limestones. They have been crosscut by the northeast-trending Turquoise Ridge shear zone and northwest-trending shear zones. Gold mineralization occurs at depths from 427 to 671 m (1,400to 2,200 ft) along the intersection of these structures. Large tonnage, flat-lying deposits occur where folded, favorable beds are intersected by the faults. The carbonate in the beds has been replaced with silica, pyrite and arsenic sulfides.
Citation

APA: E. J. Berentsen  (1996)  Discovery and Geology of the Turquoise Ridge Gold Deposit

MLA: E. J. Berentsen Discovery and Geology of the Turquoise Ridge Gold Deposit. Society for Mining, Metallurgy & Exploration, 1996.

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