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Volume 28 Issue 3
Jun 2017
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Xuebing Zhang, Keyong Wang, Chengyang Wang, Wen Li, Qi Yu, Yicun Wang, Jianfeng Li, Duo Wan, Guanghuan Huang. Age, Genesis, and Tectonic Setting of the Mo-W Mineralized Dongshanwan Granite Porphyry from the Xilamulun Metallogenic Belt, NE China. Journal of Earth Science, 2017, 28(3): 433-446. doi: 10.1007/s12583-016-0934-1
Citation: Xuebing Zhang, Keyong Wang, Chengyang Wang, Wen Li, Qi Yu, Yicun Wang, Jianfeng Li, Duo Wan, Guanghuan Huang. Age, Genesis, and Tectonic Setting of the Mo-W Mineralized Dongshanwan Granite Porphyry from the Xilamulun Metallogenic Belt, NE China. Journal of Earth Science, 2017, 28(3): 433-446. doi: 10.1007/s12583-016-0934-1

Age, Genesis, and Tectonic Setting of the Mo-W Mineralized Dongshanwan Granite Porphyry from the Xilamulun Metallogenic Belt, NE China

doi: 10.1007/s12583-016-0934-1
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  • The Xilamulun molybdenum polymetallic metallogenic belt in eastern Inner Mongolia forms one of the most important Mo metallogenic belts in northeastern China. The Dongshanwan porphyry Mo-W polymetallic deposit, in the northeastern part of the Xilamulun metallogenic belt, occurs along the periphery of a granite porphyry and consists of Mo-W-Ag sulfide and oxide disseminations and veinlets in hydrothermal assemblages. LA-ICP-MS zircon U-Pb dating of the Dongshanwan granite porphyry yields a crystallization age of 142.15±0.91 Ma, whereas molybdenite Re-Os isotopic dating model ages are of 139.9-141.5 Ma and an isochron age is of 140.5±3.2 Ma (MSWD=1.2). The age consistency indicates that the Dongshanwan deposit was a product of Early Cretaceous magmatism. The Dongshanwan granite porphyry is a high-alkali high-potassium intrusion and has high SiO2 (75.39 wt.%-76.15 wt.%), low Al2O3 (12 wt.%-13 wt.%), Ba, Ti, P, and Sr contents, with negative Eu anomalies. The Y/Nb ratios are comparable to those of average continental crust and island arc basalts, corresponding to type-A2 granites. Our geochemical data indicate that the granite porphyry emplaced in an Early Cretaceous post-orogenic extensional environment following Mongol-Okhotsk oceanic subduction and subsequent continental collision.

     

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