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Wei Mei,Xinbiao Lü,Zhi Liu,Rankun Tang,Zhilong Ai,Xiangdong Wang,Mamady Cisse 한국지질과학협의회 2015 Geosciences Journal Vol.19 No.1
Huanggang skarn Fe-Sn deposit is located in themain ridge Sn-polymetallic metallogenic sub-belt of the SouthernGreat Xing’an Range. A combination of zircon U-Pb age, geochemistryand Hf isotopic composition are reported for the orerelatedgranite (K-feldspar granite) of the Huanggang deposit toconstrain its petrogenesis and tectonic setting. LA-ICP-MS U-PbZircon dating results indicate that the K-feldspar granite wasintruded at 145.3 ± 1.6Ma. The K-feldspar granites belong to high-K calc-alkaline and shoshonite series, mainly peraluminous. Theserocks have a negative slope from La to Lu with strongly negativeEu anomalies, they demonstrate negative Ba, Sr P, Ti and Nbspikes and positive Th, U, Nd spikes on the normalized incompatibleelement diagrams. The regional geological setting togetherwith the geochemistry of the K-feldspar granite indicates that it isformed in a post-orogenic setting. The zircon Hf isotopic compositions(εHf(t): +5.2 to +6.6, 176Hf/177Hf: 0.282837‒0.282876) indicateboth juvenile crust sources that originated from depleted mantleand some ancient continental crust sources contributed to its origin,and there is a significant addition of juvenile crust under theSouthern Great Xing’an Range during the time from Paleo-Neoproterozoicto Phanerozoic.