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- W2364783321 abstract "The existence of the special apatite-orthopyroxene association in the felsic gneiss of the Larsemann Hills,east Antarctica,suggests the granulite facies metamorphism of the gneiss.The concomitant fluid-absent partial melting in the felsic gneiss was responsible for the melt segregation and residues which were favorable for the formation of Ap-Opx.The residual minerals like apatite and ilmenite are enriched in REE and have strongly affected the REE patterns of the rocks.The presence of the Ap-Opx assemblage implies the existence of appropriate but insufficient effective CaO component in the system.The crystallization of minerals in order of apatite,magnetite-ilmenite,garnet and orthopyroxene has demonstrated the changing mobile-residual components and progressive dehydration in the high-grade metamorphism.The metamorphic felsic rock rich in Ap-Opx is the unique rock derived in metamorphism,with no corresponding protolith." @default.
- W2364783321 created "2016-06-24" @default.
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- W2364783321 date "2011-01-01" @default.
- W2364783321 modified "2023-09-25" @default.
- W2364783321 title "Petrological implications of the apatite-orthopyroxene association in the high-grade felsic gneiss of the Larsemann Hills,East Antarctica" @default.
- W2364783321 hasPublicationYear "2011" @default.
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