CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES, cilt.6, sa.2, ss.139-147, 2014 (SCI-Expanded)
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).