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Authors
Affiliations
1 Department of Geology, University of Rajasthan, Udaipur 313 001, IN
2 Department of Metallurgical Engineering, M. R. Engineering College, Jaipur 302004, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 21, No 9 (1980), Pagination: 425-431
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.