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Age, genesis, and tectonic setting of the Mo-W mineralized Dongshanwan granite porphyry from the Xilamulun metallogenic belt, NE China

  • Petrogeochemistry and Geochronology
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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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Acknowledgments

This study was supported by the Opening Foundation of the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (No. GPMR201307). The authors are most grateful to the staff of the State Key Laboratory of Geological Processes and Mineral Resources (China University of Geosciences, Wuhan) as well as the Institute of Geology and Geophysics, Chinese Academy of Sciences during the zircon U-Pb dating, geochemical analyses and Re-Os isotopic analyses. The final publication is available at Springer via http://dx. doi.10.1007/s12583-016-0934-1.

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Authors and Affiliations

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

    Xuebing Zhang, Keyong Wang, Yicun Wang & Duo Wan

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

    Chengyang Wang

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

    Wen Li & Guanghuan Huang

  4. Heilongjiang Institute of Regional Geology Survey, Harbin, 150080, China

    Qi Yu

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

    Jianfeng Li

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  1. Xuebing Zhang
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Correspondence to Keyong Wang.

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Zhang, X. B., Wang, K. Y., Wang, C. Y., et al., 2017. Age, Genesis, and Tectonic Setting of the Mo-W Mineralized Dongshanwan Granite Porphyry from the Xilamulun Metallogenic Belt, NE China. Journal of Earth Science, 28(3): 433-446. doi:10.1007/s12583-016-0934-1. http://en.earth-science.net

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Zhang, X., Wang, K., Wang, C. et al. Age, genesis, and tectonic setting of the Mo-W mineralized Dongshanwan granite porphyry from the Xilamulun metallogenic belt, NE China. J. Earth Sci. 28, 433–446 (2017). https://doi.org/10.1007/s12583-016-0934-1

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  • DOI: https://doi.org/10.1007/s12583-016-0934-1

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