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A Note on the Metamorphic Conditions of Ultramafic Rocks from the Sargur Region, Karnataka, India


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1 Department of Geology, University of Mysore, Manasa Gangotri, Mysore 570006, India
     

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Ultramafic rocks occurring within the high-grade schistose rocks from the Sargur region show evidences of recrystallization. A metamorphic temperature of the order of 700± 20°C is estimated based on coexisting olivine-spinel and orthopyroxene clinopyroxene mineral chemistry.
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  • A Note on the Metamorphic Conditions of Ultramafic Rocks from the Sargur Region, Karnataka, India

Abstract Views: 188  |  PDF Views: 4

Authors

C. Srikantappa
Department of Geology, University of Mysore, Manasa Gangotri, Mysore 570006, India

Abstract


Ultramafic rocks occurring within the high-grade schistose rocks from the Sargur region show evidences of recrystallization. A metamorphic temperature of the order of 700± 20°C is estimated based on coexisting olivine-spinel and orthopyroxene clinopyroxene mineral chemistry.