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2018 Vol. 24, No. 6
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Xinwen CAO, Xiumin MA, Shuyun GONG, Youliang JI, Chunbo FANG, Zhen LI, Wei DU. A STUDY ON DISTRIBUTION CHARACTERISTICS AND ACTIVITY OF NORTH-WEST FAULTS IN SHENZHEN[J]. Journal of Geomechanics, 2018, 24(6): 759-767. doi: 10.12090/j.issn.1006-6616.2018.24.06.078
Citation: Xinwen CAO, Xiumin MA, Shuyun GONG, Youliang JI, Chunbo FANG, Zhen LI, Wei DU. A STUDY ON DISTRIBUTION CHARACTERISTICS AND ACTIVITY OF NORTH-WEST FAULTS IN SHENZHEN[J]. Journal of Geomechanics, 2018, 24(6): 759-767. doi: 10.12090/j.issn.1006-6616.2018.24.06.078
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A STUDY ON DISTRIBUTION CHARACTERISTICS AND ACTIVITY OF NORTH-WEST FAULTS IN SHENZHEN

  • 1.

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

  • 2.

    College of Earth Science, China University of Peotroleum, Beijing 102249, China

  • 3.

    School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, China

  • 4.

    Shenzhen Geology Bureau, Shenzhen 518028, Guangdong, China

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Received Date:  03 July 2017
Revised Date:  21 October 2018
    Abstract
  • The faults in Shenzhen constitute a complex grid-shaped fault system, mainly dominated by multiple secondary faults interlacing with each other in the NE-trending Wuhua-Shenzhen fault zone (WSFZ) and the NW-trending Pearl River Mouth fault zone (PRMFZ) and several WE-trending faults cutting through. WSFZ and PRMFZ are both seimogenic structures now. Series of seismogenic events occurred in Shenzhen and Pearl River Mouth indicate that structural movements are still active in the joint of NE and NW faults, which has been prove by several intense quake events during the past hundreds of years. This paper is focused on the NW-trending faults' activity in Quaternary. The distribution characteristics and activity of the NW-trending faults in Shenzhen are analyzed and summarized by means of field fault tracing, investigation of fault features, existing borehole and geophysical data collection. The results show that NW-trending faults spatially controls the Pearl River Mouth sag and regionally cuts through NE-trending faults, with poor spatial distribution continuity. The NW-trending faults were lately activated during the upper and middle Pleistocene, most of which were old faults with new movements, and recent movements happened with obvious intervals. Movements apparently weakened during the Holocene, and most secondary faults were hardly active or inactive.
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