Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (5): 1338-1349.doi: 10.13278/j.cnki.jjuese.20190092

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Petrogenesis and Tectonic Setting of Moyite in Suotuhan Area, Northern Great Xing'an Range

Yang Xiaopeng1,2, Wang Changbing3, Li Wenqing1,4   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Oil and Gas Survey, China Geological Survey, Beijing 100083, China;
    3. No. 209 Geological Party, Geological Bureau of Yunnan Nuclear Industry, Kuming 650031, China;
    4. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130061, China
  • Received:2019-04-18 Online:2019-09-26 Published:2019-10-10
  • Supported by:
    Supported by National Natural Science Foundation of China (41872234)

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Abstract: In this research, the whole-rock geochemistry and zircon U-Pb isotope chronology of moyite from Suotuhan area in the northern Great Xing'an Range are studied and their petrogenesis and tectonic significance are discussed. The LA-ICP-MS zircon U-Pb dating shows that the moyite formed in the Early Cretaceous with the ages of (139.50±0.56) Ma. The geochemical characteristics suggest that the Suotuhan moyite belongs to high K calcalkaline A type granite, and it is featured by high content of SiO2 and alkaline, and low content of CaO and MgO. The moyite has high rare earth elements (REE), and is relatively rich in LREEs with distinct negative Eu anomalies in chondrite-normalized REE diagram, which is characterized by right oblique and ‘V’-shape. The Suotuhan alkali feldspar granite is a weakly peraluminous A-type granite derived from partial melting of crustal material. The regional geological characteristics indicate that the formation of the moyite was related to lithospheric extension caused by closure of the Mongol-Okhotsk Ocean.

Key words: Suotuhan area, moyite, zircon U-Pb age, Early Cretaceous, extension environment, Northern Great Xing'an Range

CLC Number: 

  • P581
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