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Charnockites from Hullahalli, Mysore District, Karnataka State


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1 Department of Geology, University of Mysore, Manasagangotri, Mysore, India
     

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Charnockites have been noticed in the canal sections near Hullahalli, south of Mysore city. From their field, petrographic and chemical character, it is argued that they were formed as a result of granulite grade metamorphism and migmatization of pelites and intercalated earlier basic igneous rocks and pelites of the Sargur schist complex.
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  • Charnockites from Hullahalli, Mysore District, Karnataka State

Abstract Views: 217  |  PDF Views: 2

Authors

A. S. Janardhan
Department of Geology, University of Mysore, Manasagangotri, Mysore, India
H. M. Ramachandra
Department of Geology, University of Mysore, Manasagangotri, Mysore, India

Abstract


Charnockites have been noticed in the canal sections near Hullahalli, south of Mysore city. From their field, petrographic and chemical character, it is argued that they were formed as a result of granulite grade metamorphism and migmatization of pelites and intercalated earlier basic igneous rocks and pelites of the Sargur schist complex.