Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (1): 112-128.doi: 10.13278/j.cnki.jjuese.20180169

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Genesis and Tectonic Significance of Late Jurassic Granitoids in Chaihe Region, Central Great Xing'an Range, NE China

Shi Lu1, Tang Zhen1, Zheng Changqing2, Qin Tao1, Zhang Lidong1, Wang Yan1, Qian Cheng1, Yang Fan1   

  1. 1. Shenyang Center, China Geological Survey, Shenyang 110034, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2018-06-26 Published:2020-02-11
  • Supported by:
    Supported by Project of China Geological Survey (DD20190039-03,DD20160048-02,1212011120654)

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Abstract: The authors studied the Late Jurassic granitoids in the Chaihe region of central Great Xing'an Range. The Late Jurassic granitoids consist of granodiorite, monzonitic granite, and alkali-feldspar granite in lithology. We obtained two LA-ICP-MS zircon U-Pb ages of monzonitic granite, they are (152±1) Ma and (150±1) Ma respectively. The chemical analyses show that the Late Jurassic granitoids are classified as ferrous alkali-calcic rocks, and are characterized by enrichment in light rare earth elements (LREEs), large ion lithophile elements (LILEs), Zr, Hf, and depletion of heavy rare earth elements (HREEs), high field strength elements (HFSEs), Ba, and Sr, with weak to moderate Eu negative anomalies. All the geochemical characteristics suggest that the Late Jurassic granitoids were derived from the partial melting of lower juvenile crustal basaltic rocks. We propose that the generation of the Late Jurassic granitoids is related to the transitional environment of extrusion-extension after the final closure of the Mongol-Okhotsk Sea and subsequent continental thickening.

Key words: Central Great Xing'an Range, Late Jurassic, granitoids, U-Pb dating, petrogenesis, transition setting

CLC Number: 

  • P588.1
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