Partial melting mechanisms of peraluminous felsic magmatism in a collisional orogen: an example from the Khondalite belt, North China craton

Sedimentary-derived (S-type) granites are an important product of orogenic metamorphism, and a range of subtypes can be recognized by differences in field occurrence, mineralogy and geochemistry. These subtypes can reflect variations of initial protolith composition, partial melting reactions, press...

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Bibliografski detalji
Glavni autori: Huang, G, Liu, H, Guo, J, Palin, RM, Zou, L, Cui, W
Format: Journal article
Jezik:English
Izdano: Wiley 2024