Volume 24 Issue 5
Oct.  2018
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Article Navigation >  Journal of Geomechanics  > 2018  >  24(5): 607-616
ZHANG Lichen, WU Kongyou, HE Wenjun, et al., 2018. STRUCTURAL CHARACTERISTICS AND DIAGENETIC SEALING OF FAULTS IN THE BEISANTAI SWELL, JUNGGAR BASIN. Journal of Geomechanics, 24 (5): 607-616. DOI: 10.12090/j.issn.1006-6616.2018.24.05.061
Citation: ZHANG Lichen, WU Kongyou, HE Wenjun, et al., 2018. STRUCTURAL CHARACTERISTICS AND DIAGENETIC SEALING OF FAULTS IN THE BEISANTAI SWELL, JUNGGAR BASIN. Journal of Geomechanics, 24 (5): 607-616. DOI: 10.12090/j.issn.1006-6616.2018.24.05.061
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STRUCTURAL CHARACTERISTICS AND DIAGENETIC SEALING OF FAULTS IN THE BEISANTAI SWELL, JUNGGAR BASIN

doi: 10.12090/j.issn.1006-6616.2018.24.05.061
  • 1.

    School of Geosciences, China University of Petroleum, Qingdao 266580, Shandong, China

  • 2.

    Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay 834000, Xinjiang, China

More Information
  • Received: 2017-12-12
  • Revised: 2018-04-08
  • Published: 2018-10-01
    Abstract
  • A fault has a complex internal structure, which can be divided into slip damage zone and induced fracture zone. The internal diagenesis of the fault zone is widely developed, and the cementation is the most important diagenesis in the induced fracture zone on both sides of the fault, which plays an important role in the vertical sealing of the fault. The structure of the main faults in the Beisantai swell is divided quantitatively by using seismic, logging and core information, and diagenetic cementation of fault zone is studied through core observation and microscope observation of thin section. The results show that the cementation of fault zone is obvious and there are various types of cement, mainly calcite; clay minerals, zeolite, quartz and other cement are also found in fractures. Compared with the derived faults, the fracture filling and cementation of large main faults are more intense, and the sealing performance of the oil and gas is stronger. The identification under microscope and the uniform temperature test of fluid inclusion suggest that there were at least three periods of great fluid activities in the Beisantai swell, and the multiple fluid activities lead to the diagenetic sealing of the faults in this area.

     

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