Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (4): 1082-1097.doi: 10.13278/j.cnki.jjuese.20200265

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Petrogenesis and Tectonic Implication of Late Paleozoic I-A Type Granites in the Northwest Heilongjiang Province

Sun Chao1, Gou Jun1, Sun Deyou1,2, Feng Zhao1, Tian Li1   

  1. 1. College of Earth Science, Jilin University, Changchun 130061, China;
    2. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130061, China
  • Received:2021-03-26 Online:2021-07-26 Published:2021-08-02
  • Supported by:
    Supported by the National Natural Science Foundation of China (41502045) and the Nuclear Industry 243 Brigade Project of China Nuclear Industry Geological Bureau (202003)

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Abstract: Petrology, geochemistry and U-Pb geochronology of the Great Xing'an Range Tayuan and the Little Xing'an Range Erzhan Country granites in the northwest Heilongjiang Province were undertaken to determine the subduction and collisional processes of the Paleo-Asian Ocean. The Tayuan granites are mainly biotite monzogranites with zircon U-Pb age of 308 Ma, which is a Late Carboniferous intrusion, and they are characterized by high silica and total alkali contents, enrichment in light rare earth elements (LREE) and large ion lithophile elements (LILE), depletion in heavy rare earth elements (HREE) and high field strength elements (HFSE). Zircons from the Tayuan monzogranites have εHf(t) values ranging from 0.8 to 2.5, suggesting that the granitic magmas were generated by partial melting of newly-accreted lower crust. The Erzhan Country granites are dominantly monogranite and alkali-feldspar granite with zircon U-Pb ages of 305 Ma and 293 Ma. They have high silica and total alkali contents, and are characterised by enrichment in LREEs and LILE relative to HREE and HFSE, implying that they were generated by the melting of juvenile continental crust. The Late Carboniferous monogranites belong to I-type granite, and the Early Permian alkali-feldspar granite is typical A-type granite. Zircon δEu ratios can be used to estimate the melting depths of granites:The formation depth of Tayuan monzogranite and Erzhan Country monzogranite is 38.8 km and 34.7 km,respectively,while the alkali-feldspar granite formed at a shallow depth of 28.7 km. The crustal thinning during the Late Carboniferous to Early Permian might record the tectonic transition from subduction to post-collisional extension related to the final closure of the Paleo-Asian Ocean.

Key words: U-Pb geochronology, geochemistry, I-type granite, A-type granite, Paleo-Asian Ocean, the northwest of Heilongjiang Province

CLC Number: 

  • P595
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