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- W2000951508 abstract "Oxygen and strontium isotope data indicate that the primary magma of the Yangchuling Complex resulted from the mixing of upper mantle materials with crustal materials. Under reducing environment with an oxygen fugacity off 1013 bar, the magma began to crystallize at a depth of 8km between 1000°–1180°C, forming granodiorite and monzonitic granite porphyry. When the upper portion of the monzonitic granite porphyry became solidified, while its lower part remained to be liquid, explosion occurred due to pressure decrease, resulting in the formation of explosion breccia and autoclastic phenomenon, providing channels for the migration of hydrothermal solutions and favorite space for ore precipitation. The complex belongs to the calc-alkaline series. Various rock types were emplaced one after another during the process of constant differentiation from a common magma. As indicated by sulfur isotope data, the hydrothermal solutions were derived, for the most part, from the magma with only a small fraction coming from meteoric waters. Ore-forming components, including those leached out of the country rocks, carried by the solutions gave rise to W-Mo enrichment upon second boiling due to pressure drop." @default.
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- W2000951508 date "1986-01-01" @default.
- W2000951508 modified "2023-09-26" @default.
- W2000951508 title "Magmatic process and geochemistry of Yangchuling calc-alkaline complex, Jiangxi Province" @default.
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- W2000951508 doi "https://doi.org/10.1007/bf02872060" @default.
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