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Mineralogy and geochemistry of granitoids from Kinnaur region, Himachal Higher Himalaya, India: Implication on the nature of felsic magmatism in the collision tectonics
Proceedings of the Indian Academy of Sciences, Earth and Planetary Sciences
Felsic magmatism in the southern part of Himachal Higher Himalaya is constituted by Neoproterozoic granite gneiss (GGn), Early Palaeozoic granitoids (EPG) and Tertiary tourmaline-bearing leucogranite (TLg). Magnetic susceptibility values (<3×10 −3 SI), molar Al 2 O 3 /(CaO+Na 2 O+K 2 O) (≥1.1), mineral assemblage (bt-ms-pl-kf-qtz ± tur ± ap), and the presence of normative corundum relate these granitoids to peraluminous S-type, ilmenite series (reduced type) granites formed in a syncollisionaldoi:10.1007/s12040-016-0748-0 fatcat:hmyxabxf45awfnyzega2ss7gbu