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SHRIMP zircon UPb dating, geochemistry and SrNdHf isotopes of the Tongcun ore-bearing porphyry in NW Zhejiang Province, South China
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文摘
The Tongcun porphyry was emplaced at 168.7 ± 2.8 Ma according to SHRIMP UPb dating. Three porphyries in the Tongcun deposit area are most likely I-type granites. They were possibly formed in a volcanic arc regime and underwent fractional crystallization. SrNdHf isotopes imply a mixed source of ancient crust and 30–50% juvenile components. They probably lack metallogenic potential to form a giant porphyry Cu deposit.

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