Oxygen isotope ratio of quartz veins from the auriferous Ramagiri–Penakacherla schist belt and surrounding granitoids in the Eastern Dharwar craton: A case for a possible link between gold mineralization and granite magmatism

Author:

Bhattacharya Sourabh,Panigrahi M.K.,Sachan H.K.,Kharya Aditya

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference63 articles.

1. The stable isotopic evolution of a metamorphic complex, Naxos, Greece;Baker;Contrib. Mineral. Petrol.,1995

2. Bhattacharya, S., 2014. Granitic magmatism and late-stage fluid activity vis-à-vis gold mineralization in schist belts in parts of the Eastern Dharwar Craton, India (Unpub. Ph.D. Thesis, Indian Institute of Technology, Kharagpur, India, 203 pp.).

3. Heterogeneity in fluid characteristics in the Ramagiri–Penakacherla sector of the Eastern Dharwar craton: implications to gold metallogeny;Bhattacharya;Russ. Geol. Geophys.,2011

4. Granitic magmatism in the Ramagiri–Penakacherla sector of the Eastern Dharwar craton and its possible role in gold metallogeny: constraints from mineral chemistry;Bhattacharya;Mineral. Petrol.,2014

5. Mineral thermobarometry and fluid inclusion studies on the Closepet Granite, Eastern Dharwar craton, South India: implications to emplacement and evolution of late-stage fluid;Bhattacharya;J. Asian Earth Sci,2014

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