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Petrogenesis of the Perinthatta Anorthosite, Northern Kerala, 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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