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Petrogenesis of the Perinthatta Anorthosite, Northern Kerala, India


Affiliations
1 Department of Marine Geology and Geophysics, Cochin University of Science & Technology, Cochin - 682 016, India
     

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The anorthosite pluton has textural and trace element characteristics typical of a magmatic cumulate. A soda-rich intermediate magma is inferred to be the parent. Rare earth element based modelling shows that the anorthosite was derived from a parental melt having hundred times chondritic REE with a slightly fractionated pattern probably derived by the melting of granulitic or edogitic source.

Keywords

Petrogenesis, Anorthosite, Proterozoic Magmatism, Kerala.
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  • Petrogenesis of the Perinthatta Anorthosite, Northern Kerala, India

Abstract Views: 185  |  PDF Views: 2

Authors

C. G. Nambiar
Department of Marine Geology and Geophysics, Cochin University of Science & Technology, Cochin - 682 016, India
K. P. Soney
Department of Marine Geology and Geophysics, Cochin University of Science & Technology, Cochin - 682 016, India
M. Radhakrishna
Department of Marine Geology and Geophysics, Cochin University of Science & Technology, Cochin - 682 016, India

Abstract


The anorthosite pluton has textural and trace element characteristics typical of a magmatic cumulate. A soda-rich intermediate magma is inferred to be the parent. Rare earth element based modelling shows that the anorthosite was derived from a parental melt having hundred times chondritic REE with a slightly fractionated pattern probably derived by the melting of granulitic or edogitic source.

Keywords


Petrogenesis, Anorthosite, Proterozoic Magmatism, Kerala.