1996•Journal of the Geological Society of IndiaRequires access

Carbonatite Dykes from Kudangulam Area, Near Cape Comorin, Tamil Nadu

Ramachandran Ramasamy

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Abstract

Abstract Occurrence of dyke rocks of carbonatites in charnockites and granite gneisses near Kudangulam village situated 20 km NE of Cape Comorin, Tamil Nadu is reported. Petrography and Chemical composition of these rocks reveal that coarse grained curbonatites were formed under subvolcanic miarolitic crystallization from a degassed carbonatitic melt.

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Abstract Occurrence of dyke rocks of carbonatites in charnockites and granite gneisses near Kudangulam village situated 20 km NE of Cape Comorin, Tamil Nadu is reported. Petrography and Chemical composition of these rocks reveal that coarse grained curbonatites were formed under subvolcanic miarolitic crystallization from a degassed carbonatitic melt.

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Available abstract

Abstract Occurrence of dyke rocks of carbonatites in charnockites and granite gneisses near Kudangulam village situated 20 km NE of Cape Comorin, Tamil Nadu is reported. Petrography and Chemical composition of these rocks reveal that coarse grained curbonatites were formed under subvolcanic miarolitic crystallization from a degassed carbonatitic melt.

Key concepts: Carbonatite, Geology, Tamil, Cape, Geochemistry, Archaeology, Geography, Mantle (geology)

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