Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (4): 1064-1081.doi: 10.13278/j.cnki.jjuese.20200262

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Geochronology,Geochemistry and Genesis of Igneous Rocks Associated with Dayangshan Mo Deposit in Great Xing'an Range

Yang Yuanjiang1, Deng Changzhou2, Li Chenglu1, Zhang Li1, Gao Yongzhi1, Yu Xihuan1   

  1. 1. Heilongjiang Institute of Natural Resources Survey, Harbin 150036, China;
    2. Institute of Geochemistry Chinese Academy of Sciences, Guiyang 550081, China
  • Received:2020-11-11 Online:2021-07-26 Published:2021-08-02
  • Supported by:
    Supported by the Project of China Geological Survey (1212011085233), the Scientific Research Project, Bureau of Geology and Mineral Resources of Heilongjiang Province(2020-1) and the Land and Resources Public Welfare Project of Heilongjiang Province (GY-2018003)

Abstract: The geochronology and geochemistry of Mesozoic intrusions in the Dayangshan Mo deposit in the Northeastern part of the Great Xing'an Range are studied in this paper, and the petrogenesis and tectonic setting are discussed. The U-Pb dating of the medium fine-grained granite using (LA-ICP-MS) is (177.3 ±2.6) Ma and (176.5 ±1.6) Ma, namely the Early Jurassic. The dating of the diorite porphyry is (158.0 ±2.7) Ma, that is, the Late Jurassic. The study of geochemistry shows that the medium fine-grained granite is characterized by its high Si, rich K poor Fe, Mn, and Mg. It is depleted of HFSE (such as Nb, Zr, P, Th, and HREE), and rich in LILE (such as Rb, K, and LREE), with a significant negative Eu anomaly (δEu=0.39). Combined with its low Cr, Ni, Co contents and low Mg#, the medium fine-grained granite came from a source of lower crust. The diorite porphyry is relatively rich in Na,K,and alkaline, and the contents of Ca, Ti,and Mg are medium. It is rich in LILE (such as, Rb, K, and Sr) and depleted of HFSE (such as, Nb, Ta, Ti, Th, and HREE), indicating the characteristics of arc magmatic rocks in subduction zone. Combined with previous studies, we believe that the formation of medium fine-grained granite and diorite porphyry is influenced by the subduction of the Mongolian-Okhotsk Ocean, and the closing time of the residual Mongolian-Okhotsk Ocean in the Northeast of Great Xing'an Range can be limited to the Late Jurassic-Early Cretaceous.

Key words: intrusive rocks, U-Pb dating, geochemistry, Mesozoic, Dayangshan Mo deposit, NE Great Xing'an Range

CLC Number: 

  • P581
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