Hydrothermal Evolution of the Copler Porphyry-Epithermal Au Deposit, Erzincan Province, Central Eastern Turkey

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Imer A., Richards J. P., Muehlenbachs K.

ECONOMIC GEOLOGY, cilt.111, sa.7, ss.1619-1658, 2016 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 111 Sayı: 7
  • Basım Tarihi: 2016
  • Doi Numarası: 10.2113/econgeo.111.7.1619
  • Dergi Adı: ECONOMIC GEOLOGY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.1619-1658
  • Orta Doğu Teknik Üniversitesi Adresli: Evet

Özet

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.