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    Volume 44 Issue 6
    Jun.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(6): 2039-2051
    Zhang Xiong, Zhao Xiaoyan, Yang Zhusen, 2019. Thermal History of Nianzha Gold Deposit: Constraints from Zircon U-Pb, (U-Th)/He and Apatite Fission Track Geochronology. Earth Science, 44(6): 2039-2051. doi: 10.3799/dqkx.2018.379
    Citation: Zhang Xiong, Zhao Xiaoyan, Yang Zhusen, 2019. Thermal History of Nianzha Gold Deposit: Constraints from Zircon U-Pb, (U-Th)/He and Apatite Fission Track Geochronology. Earth Science, 44(6): 2039-2051. doi: 10.3799/dqkx.2018.379
    shu

    Thermal History of Nianzha Gold Deposit: Constraints from Zircon U-Pb, (U-Th)/He and Apatite Fission Track Geochronology

    doi: 10.3799/dqkx.2018.379
    • 1.

      Beijing Institute of Geology for Mineral Resources, Beijing 100012, China

    • 2.

      Key Laboratory of Earth Probe and Geodynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

    • Received Date: 2018-08-19
    • Publish Date: 2019-06-15
      Abstract
    • The Nianzha gold deposit, located in the central section of the Yurlung-Zangbo suture zone is a large orogenic gold deposit which occurred in a fracture zone bordered by altered diorite in the hanging wall to the north and the Renbu tectonic mélange in the footwall to the south. In this paper, it combines zircon U-Pb, (U-Th)/He and apatite fission track dating of the fresh and mineralized diorite in order to restrict the cooling and denudation history of the Nianzha deposit. The results show that the zircon U-Pb age of the fresh diorite is (46.32±0.53) Ma and zircon (U-Th)/He ages of fresh diorite is between (7.14 ±0.24) Ma and (9.80 ±0.27) Ma, and the zircon (U-Th)/He ages of the mineralized diorite are between (8.38±0.24) Ma and (11.19±0.31) Ma. The apatite fission track ages of two mineralization diorite are (5.9±0.5) Ma and (5.3±1.0) Ma respectively. Since the consolidation of the diorite, the Nianzha gold deposit has experienced two rapid cooling processes:the first process started from 46.3 Ma to 43.6 Ma, and the temperature dropped from 750℃ to 350℃ with the cooling rate of about 148℃/Ma, while the second process happened between 8.5~2.0 Ma with the temperature dropped from 200℃ to 30℃ with cooling rate of about 26℃/Ma. The mineralization depth of the Nianzha deposit is about 9.7 km; at 8.5 Ma, the deposit was uplifted to 4.6 km; from 8.5 to 5.6 Ma, the deposit are uplifted to 2.8 km; and from 5.6 to 2.0 Ma, the Nianzha deposit was exfoliated to the surface.

       

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