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- W2367209383 abstract "Baimanshan intrusion in the Shizishan orefield is composed of gabbrodiorite. Through the study on the petrology and geochemistry, it is considered that it is predominantly alkaline-rich, high-K calc-alkaline and metaluminous (ACNK= 063～072), it is rich in LILE (Such as Ba and Sr) and LREE, which has strong negative anomalies (Such as Nb, Ta and Ti) and slightly negative SrNd anomalies with EMI-type. It is suggested that the EMI mantle upflowed and melted the lower crust to form these rocks mainly through crystal-fractionation in extension setting." @default.
- W2367209383 created "2016-06-24" @default.
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- W2367209383 date "2004-01-01" @default.
- W2367209383 modified "2023-09-22" @default.
- W2367209383 title "Geochemical characteristics and genetic mechanism of the Baimangshan intrusions in the Shizishan orefield, Anhui Province" @default.
- W2367209383 hasPublicationYear "2004" @default.
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