Volume 25 Issue S1
May  2019
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Article Navigation >  Journal of Geomechanics  > 2019  >  25(S1): 170-174
ZHU Weiping, ZHU Hongwei, XU Luping, et al., 2019. CHARACTERISTICS OF AERO GRAVITY AND MAGNETISM REMOTE SENSING AND CORRELATION ANALYSIS OF FAULT STRUCTURES IN HAMI SHAQUANZI AREA, XINJIANG. Journal of Geomechanics, 25 (S1): 170-174. DOI: 10.12090/j.issn.1006-6616.2019.25.S1.029
Citation: ZHU Weiping, ZHU Hongwei, XU Luping, et al., 2019. CHARACTERISTICS OF AERO GRAVITY AND MAGNETISM REMOTE SENSING AND CORRELATION ANALYSIS OF FAULT STRUCTURES IN HAMI SHAQUANZI AREA, XINJIANG. Journal of Geomechanics, 25 (S1): 170-174. DOI: 10.12090/j.issn.1006-6616.2019.25.S1.029
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CHARACTERISTICS OF AERO GRAVITY AND MAGNETISM REMOTE SENSING AND CORRELATION ANALYSIS OF FAULT STRUCTURES IN HAMI SHAQUANZI AREA, XINJIANG

doi: 10.12090/j.issn.1006-6616.2019.25.S1.029

  • China Aero Geophysical Survey and Remote Sensing Center for Nature and Resources, Beijing 100083, China

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  • Published: 2019-05-01
    Abstract
  • In order to study the correlation between aero geophysical survey (gravity and magnetism) and remote sensing in the study of fault structures, 18 fault structures were identified using the aero geophysical survey (gravity and magnetism) remote sensing data in Hami Shaquanzi area, Xinjiang. Based on the analysis of the characteristics and correlation of the 18 faults, the results show that the first-order and second-order faults in the area are all gravity magnetism remote sensing related. The third-order faults related to gravity magnetism are also faults in the same direction as the main structural framework. Both gravity and magnetism related and magnetism remote sensing related faults are the third-order faults. The unrelated faults are also the third-order faults. On the whole, it is more effective to identify large faults or main frame faults using gravity and magnetism remote sensing data.

     

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