Article ID Journal Published Year Pages File Type
5754513 Journal of Geochemical Exploration 2017 54 Pages PDF
Abstract
Based on the field and laboratory observation, mineral chemistries, fluid inclusion studies and isotope composition analysis, it is suggested that the Eğrikar Fe-Cu skarn mineralization occurs in a magmatic origin fluids being initially under reduced conditions, subsequently under oxidized conditions, and at shallow depth.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
Authors
, , , , , ,