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Authors
Affiliations
1 Department of Geology, Ashutosh College, Calcutta 700 026, IN
2 Department of Geology, Presidency College, Calcutta 700 073, IN
3 Department of Applied Geology, Indian School of Mines, Dhanbad 826 004, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 32, No 1 (1988), Pagination: 68-70
Abstract
Spodumence is recorded from the northern part of the Sandur Schist Belt, near T. B. Dam, Hospel The mineral occurs in a quartz-spodumene vein near the contact of the supracrustal rocks with the granitic gneisses.
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