Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

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Diagenetic Features in Sulphides of Dariba-Rajpura Deposit, Udaipur District, Rajasthan


Affiliations
1 Department of Geology, University of Rajasthan, Udaipur 313 001, India
2 Department of Metallurgical Engineering, M. R. Engineering College, Jaipur 302004, India
     

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Mineralisation is mainly confined to kyanite-graphite-quartz-mica schist, meta chert (chert and its recrystallised form) at places interbanded with quartzite, calc silicate rock, and impure marble. Sulphide ores reveal a variety of diagenetic structures: diagenetic dykes, diagenetic fracture filling, stylolite seams in sulphide-cherty rock and cementation of silicate minerals by sulphide grains.
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  • Diagenetic Features in Sulphides of Dariba-Rajpura Deposit, Udaipur District, Rajasthan

Abstract Views: 229  |  PDF Views: 2

Authors

M. K. Pandya
Department of Geology, University of Rajasthan, Udaipur 313 001, India
S. L. Solanki
Department of Metallurgical Engineering, M. R. Engineering College, Jaipur 302004, India
T. K. Pandya
Department of Geology, University of Rajasthan, Udaipur 313 001, India

Abstract


Mineralisation is mainly confined to kyanite-graphite-quartz-mica schist, meta chert (chert and its recrystallised form) at places interbanded with quartzite, calc silicate rock, and impure marble. Sulphide ores reveal a variety of diagenetic structures: diagenetic dykes, diagenetic fracture filling, stylolite seams in sulphide-cherty rock and cementation of silicate minerals by sulphide grains.