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Devaraju, J.
- P-T Conditions of Metamorphism and Fluid Inclusion Characteristics of the Coorg Granulites, Karnataka
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Affiliations
1 Department of Geology, Manasagangotri, University of Mysore, Mysore 570006, IN
1 Department of Geology, Manasagangotri, University of Mysore, Mysore 570006, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 44, No 5 (1994), Pagination: 495-504Abstract
Charnockites and basic granulites occur extensively around Coorg in Western Ghats. Minor metasedimentary rocks like kyanite/sillimanite bearing gneisses and ironstone also occur. A set of late dolerite dykes cross cut all the lithologies.
The Coorg granulites record a near-peak metamorphic conditions of 720 to 760° C at pressures of 7 lo 8.6 kb. Charnockites and basic granulites contain high-density ( 1.07 to 1.09 g/cc) carbonic inclusions. Micro-textures, mineral P-T and fluid inclusion data indicate "clockwise" P-T trajectory, pointing to a relatively rapid uplift/erosion of the Coorg granulites.
Keywords
Granulites, Thermobarometry, Fluid Inclusions, Igneous Petrology, Coorg District, Karnataka.- Metamorphic History of Staurolite-Kyanite-Garnet-Cordieritebearing Pelites of Mangalore-Mercaka Lineament, South India
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PDF Views:214
Authors
Affiliations
1 Department of Geology, University of Mysore, Manasagangotri, Mysore - 570 006
2 Department of Geology, University of Mysore, Manasagangotri, Mysore - 570 006, IN
1 Department of Geology, University of Mysore, Manasagangotri, Mysore - 570 006
2 Department of Geology, University of Mysore, Manasagangotri, Mysore - 570 006, IN