WU Shi-guo, YU Zhao-hua, ZOU Dong-bo, ZHANG Hai-ying. STRUCTURAL FEATURES AND CENOZOIC EVOLUTION OF THE TAN-LU FAULT ZONE IN THE LAIZHOU BAY,BOHAI SEA[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 101-110.
Citation: WU Shi-guo, YU Zhao-hua, ZOU Dong-bo, ZHANG Hai-ying. STRUCTURAL FEATURES AND CENOZOIC EVOLUTION OF THE TAN-LU FAULT ZONE IN THE LAIZHOU BAY,BOHAI SEA[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 101-110.
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STRUCTURAL FEATURES AND CENOZOIC EVOLUTION OF THE TAN-LU FAULT ZONE IN THE LAIZHOU BAY,BOHAI SEA

  • 1 College of Geo-Resources and Information, Petroleum University of China(Huadong), Qingdao 266555, China;

  • 2 Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;

  • 3 Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;

  • 4 Geophysical Research Institute of Shengli Oil Field, Dongying 257022, China

More Information
  • Received Date: February 17, 2006
  • Revised Date: July 14, 2006
    Graphical Abstract
    • Abstract
  • The middle portion of Tan-Lu fault zone is divided into two branches(the east and west faults) and enters the Laizhou Bay of the Bohai Sea, according to the interpretation and analysis results of the seismic lines across the study area. The structural characters of the middle portion of the Tan-Lu fault zone are little reported due to lack of seismic data. During this study, we discuss the tectonics and evolution of the Tan-Lu fault in the Laizhou Bay by using the latest seismic data. The research result shows that the two faults are different in kinematical characters in the study area:the west fault is a normal fault while the east is a strike-slip one. The Tan-Lu fault zone is the main fault in the study area. After careful researches on the stratigraphic distribution and combination, sectional shape and dimensional distribution features of the faults in the study area, the Cenozoic tectonic evolution history of the middle portion of the Tan-Lu fault zone is divided into three stages:Paleocene-Eocene extension, Oligocene-early Miocene extrusion and dextral strike-slip, middle Miocene to the present stable depression, which are mainly controlled by direction and velocity changes of the Pacific plate.
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    • References (36)
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