Volume 26 Issue 6
Dec.  2020
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Article Navigation >  Journal of Geomechanics  > 2020  >  26(6): 911-922
LIU Wen, QIU Nansheng, MA Yinsheng, et al., 2020. Distribution characteristics and genetic analysis of the abnormal fluid pressure in the middle Permian in the northern fault-fold zone of the western Sichuan Depression. Journal of Geomechanics, 26 (6): 911-922. DOI: 10.12090/j.issn.1006-6616.2020.26.06.072
Citation: LIU Wen, QIU Nansheng, MA Yinsheng, et al., 2020. Distribution characteristics and genetic analysis of the abnormal fluid pressure in the middle Permian in the northern fault-fold zone of the western Sichuan Depression. Journal of Geomechanics, 26 (6): 911-922. DOI: 10.12090/j.issn.1006-6616.2020.26.06.072
shu

Distribution characteristics and genetic analysis of the abnormal fluid pressure in the middle Permian in the northern fault-fold zone of the western Sichuan Depression

doi: 10.12090/j.issn.1006-6616.2020.26.06.072
  • 1.

    Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China

  • 2.

    Key Laboratory of Petroleum Geomechanics, China Geological Survey, Beijing 100081, China

  • 3.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 4.

    State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing 102249, China

  • 5.

    School of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

  • 6.

    Oil and Gas Resources Survey, China Geological Survey, Beijing 100083, China

More Information
  • Received: 2020-09-08
  • Revised: 2020-10-10
  • Published: 2020-12-01
    Abstract
  • The temperature and pressure field is the key point for studying on the mechanism of hydrocarbon accumulation in the petroliferous basin, and the reconstruction of paleo-pressure particularly plays an important role in the study of hydrocarbon migration and accumulation, and even diagenesis in reservoirs and hydrocarbon generation for source rocks. In this paper, with pressure distribution as constraint, the paleo-pressures in the middle Permian of the northwestern Sichuan Basin were reconstructed by adopting basin modeling. In the northwest fault-fold belt of the Sichuan Basin two stages of overpressure developed, in the middle Permian, especially from the late Jurassic to the end of early Cretaceous.The overpressure accumulated rapidly in reservoirs under the effect of compressive stress which varied greatly in different structural units. The weak overpressure developed near the orogenic belt, which recovered to normal pressure after the late Cretaceous; but the strong overpressure developed in the fold and foredeep zone far from the orogenic belt even after the structure uplift, which was mainly controlled by the external compressive stress from northwest.

     

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