Cg. Nambiar et al., PETROGENESIS OF THE PERINTHATTA ANORTHOSITE, NORTHERN KERALA, INDIA, Journal of the Geological Society of India, 50(4), 1997, pp. 501-509
The anorthosite pluton has textural and trace element characteristics
typical of a magmatic cumulate. A soda-rich intermediate magma is infe
rred to be the parent. Rare earth element based modelling shows that t
he anorthosite was derived from a parental melt having hundred times c
hondritic REE with a slightly fractionated pattern probably derived by
the melting of granulitic or eclogitic source.