Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (1): 145-164.doi: 10.13278/j.cnki.jjuese.20170229

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Petrogenesis and Geodynamic Significance of Intermediate-Basic Intrusive Rocks in Xiaokuile River, Eastern Slope of the Great Xing'an Range: Evidences of Zircon U-Pb Geochronology, Elements and Hf Isotope Geochemistry

Sun Fanting1,2, Liu Chen3, Qiu Dianming4, Lu Qian5, He Yunpeng5, Zhang Mingjie1   

  1. 1. School of Earth Sciences, Lanzhou University, Lanzhou 730000, China;
    2. Institute of Bureau of Nonferrous Metals Geological Prospecting of Jilin Province, Changchun 130012, China;
    3. School of Mechanical & Electronic Engineering, Changchun Institute of Technology, Changchun 130012, China;
    4. Jilin University, Changchun 130026, China;
    5. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2017-10-09 Online:2018-01-26 Published:2018-01-26
  • Supported by:
    Supported by National Natural Science Foundation of China(413390444)and Geological Survey Projects of China Geological Survey(12120113055200,1212011220936)

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Abstract: The most rock types are Phanerozoic granites and volcanic rocks in the Great Xing'an Range, with small amount of basic and intermediate intrusive rocks which have been reported in Tahe, Tayuan, Fuxili, Wula Mountain and Biliutai. The differences of the formation ages and petrogenesis between those rocks provide the major basis and clues in the study on the evolution of crust and mantle in the Great Xing'an Range. We observed two irregular basic masses in the granitic complexes during the basic geologic surveys in the middle of Xiaokuile River, the Honghuaerji region, the north of east slope of the Great Xing'an Range. We obtained five points by systematical researches in petrography, chronology, elements,and Hf isotopes geochemistry. The two basic rocks are composed of fine-grained bojite and gabbro diorite. We collated the single grain zircon LA-ICP-MS U-Pb dating, and concluded that the age of diagenesis is 310-293 Ma. Rocks are the transitional series of metaluminous potassic-sodium and tholeiitic-calcalkalic. The main residual minerals of the initial magma that originated by low-degree (less than 5%) partial melting of the EM derived from the metasomatism of melt-fluid are pyroxene, garnet and perovskite. The evolution of magma was mainly of fractional crystallization followed by accumulation. The basic rocks were formed in the initial environment which was under the late collision between the Songnen massif and the Xing'an plot or the initial oceanic island-late oceanic arc.

Key words: geochemistry, Hf isotopes, geochronology, petrogenesis, intermediate-basic intrusive rocks in the Xiaokuile River, eastern slope of the Great Xing'an Range

CLC Number: 

  • P618
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