Volume 22 Issue 1
Mar.  2016
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Article Contents
XU Sheng-lin, ANG Jiao-dong, ZHOU Xin-gui, et al., 2016. RELATIONSHIP BETWEEN BOHAI SEGMENT OF TANLU FAULT ZONE AND YISHU FAULT ZONE. Journal of Geomechanics, 22 (1): 56-65.
Citation: XU Sheng-lin, ANG Jiao-dong, ZHOU Xin-gui, et al., 2016. RELATIONSHIP BETWEEN BOHAI SEGMENT OF TANLU FAULT ZONE AND YISHU FAULT ZONE. Journal of Geomechanics, 22 (1): 56-65.


More Information
  • Received: 2015-10-17
  • Published: 2016-03-01
  • Based on the high-precision magnetotelluric and seismic profiles, we analyzed several fractures of Weibei hollow which was the connection point of Bohai segment Fault and Yishu Fault Belt. Furthermore, integrated with stratum forming characters, we found these fractures might belong to different fault systems. We analyzed that the fault Fa and Fb were Paleogene normal faults corresponded with the west fault and east fault of the Tan-Lu fault zone. They showed steep or gentle spoon shaped morphology and disappeared in the middle crust. They controlled Cenozoic sedimentation and the cutting site was relatively shallow. Under the Cenozoic normal fault system, there were some Mesozoic faults which was called extensional fault system. The fault F1 and F6 whose fracture surface were overall suberect control Mesozoic sedimentation with other four faults. And their cutting site was relatively deep and extending downward. Integrated with regional tectonic background and Gravity-Magnetic anomaly data, we concluded that the fault F1 and F6 connected southward with Tangwu-Gegou fault and Changyi-Dadian fault and extended northward into the deep part of Bohai Bay Basin. At the same time, these Mesozoic faults constrained clearly the formation and evolution of the shallow Paleogene fault system.


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