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Recycling of subducted upper continental crust: Constraints on the extensive molybdenum mineralization in the Qinling-Dabie orogen
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文摘
Most of the porphyry Mo ore deposits in the Qinling–Dabie orogenic belt are associated with Late Mesozoic granites. The ore-related granites were derived from partial melting of the subducted continental crust. The Mo source is related to the subducted Mo-rich sedimentary rocks.

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