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- W2355815066 abstract "The Penshan granitic body is a calc-alkaline pluton composed of muscovite alkali granite,two-mica alkali feldspar granite and biotite adamellite. It is geochemically characteristzed by rich in Si,alkali,aluminum,comparatively rich in LREE and poor in calcium,belonging to crust-source remelting granitoids. Study of lead-sulfur isotopes and REE geochemistry shows that polymetallic mineralization in the study area is of close relationship with emplacement of the Pengshan granitic body: magmatism provided not only heat source but also ore-forming materials;the deposition of metals in the Pengshan dome and its secondary structures from the metallogenetic fluid formed after crystallization differentiation resulted in mineralization. The re-activation of regional basement faults and plate collision might provide tectonic condition for Late Yanshanian magmatism." @default.
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- W2355815066 date "2004-01-01" @default.
- W2355815066 modified "2023-09-24" @default.
- W2355815066 title "Geochemical characteristics and related mineralization of Pengshan granitic body in Jiangxi Province" @default.
- W2355815066 hasPublicationYear "2004" @default.
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