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WANG Chaoqun, JIA Liyun, HU Daogong, MA Xiumin, GU Jingchao, DING Yingying, CAO Xinwen, XIA Mengmeng, WU Huanhuan. 2021. Activity of eastern part of the Maniao-Puqian fault in northern Hainan Island and its evaluation of crustal stability[J]. Geology in China, 48(2): 618-631. doi: 10.12029/gc20210219
Citation: WANG Chaoqun, JIA Liyun, HU Daogong, MA Xiumin, GU Jingchao, DING Yingying, CAO Xinwen, XIA Mengmeng, WU Huanhuan. 2021. Activity of eastern part of the Maniao-Puqian fault in northern Hainan Island and its evaluation of crustal stability[J]. Geology in China, 48(2): 618-631. doi: 10.12029/gc20210219
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Activity of eastern part of the Maniao-Puqian fault in northern Hainan Island and its evaluation of crustal stability

  • 1.

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

  • 2.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

  • 3.

    Key laboratory of Neotectonic Movement and Geohazard, , Beijing, 100081, China

  • 4.

    No. 13 Geological Party of Jiangsu Province, Jiangsu 212000, China

    • Fund Project: Supported by the project of China Geological Survey (No.DD20190306, No.DD20160269)
More Information
  • Author Bio: WANG Chaoqun, female, born in 1993, doctorial candidate, engaged in the study of active structure survey and research; E-mail: 871269501@qq.com
  • Corresponding author: JIA Liyun, female, born in 1982, assistant research fellow, engaged in the study of active structure and tectonic landform; E-mail: 158943653@qq.com 
Received Date:  20 September 2018
Revised Date:  30 January 2019
Publish Date:  25 April 2021
    Abstract

  • The Maniao-Puqian fault trending east-west, as the major one controlling the Qiongshan earthquake registered 7.5 magnitude on Richter scale in 1605, is a major active fault in the northern Hainan area. Hence, its activity's measuring is critical for crustal stability evaluation and for geological hazard forecast in the northern part of Hainan Island. Various methods were used to determine the distribution of the eastern part of this fault, including remote sensing images interpretation, fault landform mapping, high-density electrical detecting and cross-section drilling validation. The results show that it is spatially composed of 8 north-dipping or south-dipping NEE-trending normal faults (F2-1~F2-8), constituting the three-graben and two-barrier structure, and inheriting the multi-stage activities from the faults before the Pliocene. Five Holocene active faults (F2-1, F2-4, F2-6, F2-7 and F2-8), two pre-Quaternary faults (F2-2 and F2-5) and one early Miocene fault (F2-3) were identified by chronological tests. Moreover, the vertical movement rate of F2-1, F2-7 and F2-8 was 0.43-1.79 mm/a, while that of F2-4 and F2-6 between 0.12-0.33 mm/a since Holocene. The above research shows that the structures in this area are all in an active state, which has a great influence on the future engineering construction, and the monitoring efforts must be strengthened.

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