Abstract
The large-scale Huangshaping Pb-Zn-W-Sn-Mo polymetallic deposit is located in the central Nanling mineralization zone, South China. Six molybdenite samples from the Huangshaping deposit were selected for Re-Os isotope measurement in order to define the mineralization age of the deposit. It yields a Re-Os isochron age of 154.8±1.9 Ma (2σ), which is in accordance with the Re-Os model ages of 150
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