Geochemical characteristics of the Shujiadian Cu deposit related intrusion in Tongling: Petrogenesis and implications for the formation of porphyry Cu systems in the Middle-Lower Yangtze River Valley metallogenic belt, eastern China
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文摘

The geochemical and Sr–Nd–Hf–O isotopic evidence show the existence of magma mixing.

Enriched lithospheric mantle resulted from involvement of Neoproterozoic-subducted materials.

The injected mafic magma play a key role for the formation of the Shujiadian deposit.

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