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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 1995  >  17(4): 316-323
Qi Jiafu, Zhang Yiwei, Lu Kezheng, Yang Qiao, . EXTENSIONAL PATTERN AND DYNAMIC PROCESS OF THE CENOZOIC RIFTING BASIN IN THE BOHAI BAY[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(4): 316-323. doi: 10.11781/sysydz199504316
Citation: Qi Jiafu, Zhang Yiwei, Lu Kezheng, Yang Qiao, . EXTENSIONAL PATTERN AND DYNAMIC PROCESS OF THE CENOZOIC RIFTING BASIN IN THE BOHAI BAY[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(4): 316-323. doi: 10.11781/sysydz199504316
shu

EXTENSIONAL PATTERN AND DYNAMIC PROCESS OF THE CENOZOIC RIFTING BASIN IN THE BOHAI BAY

doi: 10.11781/sysydz199504316
  • 1.

    Petroleum University, Beijing

  • Received Date: 1994-07-30
  • Publish Date: 1995-10-25
    Abstract
  • The Bohai bay Basin is a Cenozoic rifting one.Based on a synthetic study of the litho-spheric structure and basinal tectonic characteristics of the basinal area,the extensional deformation of the continental lithosphere can be interpreted as a double or muliple layered extensional pattern, which is dominated by simple shear extensional deformation in the upper part and pure shear extensional deformation in the lower part. Thermal action withinthe mantle is a major factor which controls thc dynamic process of rifting extension in thebasinal area, as shown by the "event" sequences of the tectonic evolution proces,in thebasinal area. Nevertheless, the strike-slip of the deep fault is driven by regional stressfield formed by plate boundary effort transferring to the basinal area.

     

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