Magmatic Garnet and Magma Evolution in Cuonadong Leucogranites: Constraints from Petrology and Mineral Geochemistry

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چکیده

Located at the eastern segment of Tethyan Himalayan tectonic unit, Cuonadong leucogranites (muscovite granite and pegmatite) have a mineral assemblage quartz, plagioclase, alkali feldspar, as well muscovite garnet. Garnets in both pegmatite belong to almandine–spessartine solid solution, with minor andradite, grossular, pyrope, show specific Mn zoning relatively rim-ward depletion trend. However, few garnets grossular enrichment towards rim. All analyzed are characterized by HREE LREE obvious Eu anomalies. The difference is that from distinct left-declined or flat patterns, while those featured right-declined patterns. Moreover, more HREE- Y-rich cores compared granite. MnO concentration, spessartine content, MnO/(MnO + FeO) ratio dome increase pegmatite, suggesting likely formed evolved environment. Elevated CaO contents garnet rim may reflect an influence fluids their composition. major trace element compositions textures suggest magmatic origin formation moderately low temperatures low-pressure conditions. From system entered fluid-rich environment crystallized lower-temperature fluid.

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ژورنال

عنوان ژورنال: Minerals

سال: 2022

ISSN: ['2075-163X']

DOI: https://doi.org/10.3390/min12101275