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An Occurrence of Spodumene in the Sandur Schist Belt, Karnataka


Affiliations
1 Department of Geology, Ashutosh College, Calcutta 700 026, India
2 Department of Geology, Presidency College, Calcutta 700 073, India
3 Department of Applied Geology, Indian School of Mines, Dhanbad 826 004, India
 

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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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  • An Occurrence of Spodumene in the Sandur Schist Belt, Karnataka

Abstract Views: 194  |  PDF Views: 146

Authors

Abdul Matin
Department of Geology, Ashutosh College, Calcutta 700 026, India
Kamal Nandi
Department of Geology, Presidency College, Calcutta 700 073, India
Dhruba Mukhopadhyay
Department of Applied Geology, Indian School of Mines, Dhanbad 826 004, India

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.