Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (1): 261-272.doi: 10.13278/j.cnki.jjuese.20190016

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Deep and Shallow Structural Characteristics of Middle Segment of Nenjiang-Balihan Fault Based on Geophysical Data

Zhang Penghui1,2, Zhang Xiaobo1,2, Fang Hui1,2, Wang Xiaojiang1,2, Liu Jianxun1,2   

  1. 1. National Center for Geological Exploration Technology, Langfang 065000, Hebei, China;
    2. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, Hebei, China
  • Received:2019-01-23 Published:2020-02-11
  • Supported by:
    Supported by Geological Survey Project of China Geological Survey (DD20160164, DD20190030) and Fundamental Research Funds for the Central Public Research Institutes (AS2019Y02)

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Abstract: The Nenjiang-Balihan fault is an important fault on the western margin of Songliao basin. It is of great significance to study the formation and evolution of the Meso and Cenozoic basins in the region. The previous research on the deep structural characteristics of the Nenjiang-Balihan fault is relatively inadequate, as it is covered by thick sediments. In this study, one MT (magnetotelluric sounding) line and one seismic profile across the Nenjiang-Balihan fault were processed and interpreted, and in combination with the regional drilling data, the structural characteristics of the deep and shallow parts of the fault were obtained. The results show that the deep electrical structures along the MT profile are horizontally bounded by an "eight-shaped" low resistance band and corresponded well to the geological units. It is inferred that the east-dipping low-resistivity strip L3 represents the Nenjiang-Balihan fault with the characteristics of concealment, ultra-crust, shallow high angle, etc. The whole fault is composed of two east-dipping anti-Y-type faults and one west-dipping fault, in a flower-like structural style, indicating that the faults have experienced a strong compressive stress environment.

Key words: Nenjiang-Balihan fault, magnetotelluric sounding, low-resistivity layer in crust, structural characteristics, Songliao basin

CLC Number: 

  • P319.2
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