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Vogesite from Carbonatite Complex of Tiruppattur, Tamil Nadu, India


Affiliations
1 Department of Geology and Mining, Madras 32, India
 

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Vogesite occurs as a melanocratic dyke rock in close proximity to carbonatite outcrops of Sevvattur. Vogesite was formed as a late magmatic differentiate of a monzonitic magma under CO2-rich wet subvolcanic conditions. Postmagmatic fluids enriched in acidic components permeated through the rock causing development of lamprophyric character.
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  • Vogesite from Carbonatite Complex of Tiruppattur, Tamil Nadu, India

Abstract Views: 206  |  PDF Views: 146

Authors

R. Ramasamy
Department of Geology and Mining, Madras 32, India

Abstract


Vogesite occurs as a melanocratic dyke rock in close proximity to carbonatite outcrops of Sevvattur. Vogesite was formed as a late magmatic differentiate of a monzonitic magma under CO2-rich wet subvolcanic conditions. Postmagmatic fluids enriched in acidic components permeated through the rock causing development of lamprophyric character.