Microthermometric and stable isotopic (O and H) characteristics of fluid inclusions in the porphyry related Copler (Ilic - Erzincan) gold deposit, central eastern Turkey


CANBAZ O. , GÖKCE A.

CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES, vol.6, no.2, pp.139-147, 2014 (Journal Indexed in SCI) identifier identifier

  • Publication Type: Article / Article
  • Volume: 6 Issue: 2
  • Publication Date: 2014
  • Doi Number: 10.2478/s13533-012-0173-0
  • Title of Journal : CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES
  • Page Numbers: pp.139-147

Abstract

The Copler gold deposit occurs within the stockwork of quartz hosted by the Copler granitoid (Eosen) and by surrounding metasediments of Keban metamorphic (Late Paleozoic - Early Mesozoic) and the Munzur limestones (Late Carboniferous - Early Cretaceous).