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1992•Journal of the Geological Society of IndiaOpen access

Syn-Metamorphic Carbonic Inclusions in the Satnur-Halgur Granulites, Karnataka, India

C. Srikantappa

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Abstract

Abstract Peak-metamorphic carbonic pore fluids have been observed in granulite facies rocks of the Satnur-Halgur area. The CO2 densities (1.045 to 0.900 g/cc) are consistent with the P-T metamorphic conditions, indicating syn-metamorphic nature of carbonic inclusions.

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Abstract Peak-metamorphic carbonic pore fluids have been observed in granulite facies rocks of the Satnur-Halgur area. The CO2 densities (1.045 to 0.900 g/cc) are consistent with the P-T metamorphic conditions, indicating syn-metamorphic nature of carbonic inclusions.

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Available abstract

Abstract Peak-metamorphic carbonic pore fluids have been observed in granulite facies rocks of the Satnur-Halgur area. The CO2 densities (1.045 to 0.900 g/cc) are consistent with the P-T metamorphic conditions, indicating syn-metamorphic nature of carbonic inclusions.

Key concepts: Granulite, Geology, Metamorphic rock, Geochemistry, Geomorphology, Facies, Structural basin

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