Hydrothermal Evolution of the Copler Porphyry-Epithermal Au Deposit, Erzincan Province, Central Eastern Turkey
ECONOMIC GEOLOGY, vol.111, no.7, pp.1619-1658, 2016 (SCI-Expanded, Scopus)
- Publication Type: Article / Article
- Volume: 111 Issue: 7
- Publication Date: 2016
- Doi Number: 10.2113/econgeo.111.7.1619
- Journal Name: ECONOMIC GEOLOGY
- Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Page Numbers: pp.1619-1658
- Open Archive Collection: AVESIS Open Access Collection
- Middle East Technical University Affiliated: Yes
Abstract
The Copler Au deposit (measured and indicated resource of 122.8 million tonnes at 1.7 g/t Au, 4.8 g/t Ag, and 0.1 wt % Cu) is centered around shallow-level dioritic to granodioritic intrusive rocks of the middle Eocene Copler-Kabatas, magmatic complex, which have been emplaced into a succession of regionally metamorphosed late Paleozoic-Mesozoic sedimentary and carbonate rocks.