Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5754513 | Journal of Geochemical Exploration | 2017 | 54 Pages |
Abstract
Based on the field and laboratory observation, mineral chemistries, fluid inclusion studies and isotope composition analysis, it is suggested that the EÄrikar 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
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Authors
Ferkan Sipahi, İbrahim Akpınar, ÃiÄdem Saydam Eker, Abdullah Kaygusuz, Alaaddin Vural, Meltem Yılmaz,