Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (1): 113-125.doi: 10.13278/j.cnki.jjuese.201701111

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Petrogenesis of the Early Paleozoic Diorite in the Northeast Nenjiang Area: Evidence from Zircon U-Pb Chronology and Geochemistry

Qi Zhongyou1, Feng Zhiqiang2,3, Wen Quanbo2, Zhang Tiean1, Liu Binqiang2, Li Xiaoyu1, Du Bingying1   

  1. 1. Heilongjiang Province Institute of Regional Geological Survey, Haerbin 150080, China;
    2. College of Earth Science, Jilin University, Changchun 130061, China;
    3. College of Mining Engineering, Taiyuan University of Technology, Taiyuan 030024, China
  • Received:2015-12-23 Online:2017-01-26 Published:2017-01-26
  • Supported by:
    Supported bythe Natural Science Foundation of China (41602235, 41502207, 41302175) and the Project of China Geological Survey (12120114033501)

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Abstract: NE China was traditionally considered the eastern part of the Central Asian Orogenic Belt (CAOB) and was composed of different mico-blocks in the Paleozoic. There are some debates about the collision age and location between the Xing'an and Songliao-Nenjiang blocks in NE China. The discovery of the records of the Early Paleozoic magmatism is a key to solve the debates. Early Paleozoic diorites are indentified in this study in the Nenjiang area, western Heilongjiang Province. The LA-ICP-MS zircon U-Pb dating indicates an age of (435.3±1.1)Ma. The diorites have 55.01%-61.82 wt% SiO2, and 14.97%-16.67 wt% Al2O3, with Na2O+K2O=4.55%-6.94 wt%, and exhibit high Na2O/K2O and low FeOT/MgO (0.51-0.96) ratios, and moderate K2O (0.10%-2.12%), TiO2 (0.99%-1.42%), and P2O5 (0.33%-0.49%). These results indicate that the diorites belong to medium K calc-alkaline series. Their A/CNK and A/NK values range from 0.78 to 1.35 and 1.63 to 2.21 respectively,which are generally consistent with those of type I granites. The diorites display right-inclined rare earth element (REE) patterns (La/Yb)N=9.86-13.93,with relatively high total REE abundances (ΣREE=227.02×10-6-289.17×10-6), and week Eu anomalies (Eu/Eu*=0.88-1.02). In trace elements, the diorites are characterized by depletion in high field strength elements (HFSEs,such as Nb and Ti). The primary magma of the diorites in the northeast Nenjiang area was generated by partial melting of mantle wedge that had been metasomatized by subduction-related fluids. Integrating regional data and the research result of this study it is suggest that the Nenjiang diorites was formed in an active continental margin setting, resulting from subduction of the paleo Nenjiang-Heihe oceanic plate located between the Xing'an and Songliao blocks.

Key words: Early Paleozoic, diorite, U-Pb dating, geochemistry, Lesser Xing'an Range, Nenjiang area

CLC Number: 

  • P588.122
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