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How we know whether the origin of metamorphic schists and aluminous gneisses is marine sediments or immature continental sediments. What geochemical or petrological evidence is more appropriate?
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One of the distinct characteristics of S-type granites is that they are not associated with more mafic rocks contrasting to the I-type granites. May anyone explains this?
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Rare-element pegmatites are commonly assumed a fractionation product of magma from which a spatially and temporally related two-mica granite is crystallized. How this assertion is geochemically...
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Geochemical data of granite-pegmatite from my present study shows peraluminous, S-type, Low K, magnesian series, Flat REE, with Syn-COLG affinity. Garnet compositions in pelitic/gneiss county...
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