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Volume 28 Issue 3
Jun 2017
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Journal of Earth Science  > 2017  >  28(3): 433-446.
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
shu

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
  • 1.

    College of Earth Sciences, Jilin University, Changchun 130061, China

  • 2.

    Department of Earthquake Science, Institute of Disaster Prevention Science and Technology, Beijing 101601, China

  • 3.

    Inner Mongolia Shandong Gold Minerals Survey Co. Ltd., Chifeng 024005, China

  • 4.

    Heilongjiang Institute of Regional Geology Survey, Harbin 150080, China

  • 5.

    College of Urban and Environmental Sciences, Liaoning Normal University, Dalian 116029, China

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    Abstract
  • 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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