Volume 29 Issue 3
Jun.  2023
Turn off MathJax
Article Contents
Article Navigation >  Journal of Geomechanics  > 2023  >  29(3): 339-354
JIA L Y，MA X M，JING J J，et al.，2023. Dynamic variation characteristics of in-situ stress in the 1605 Qiongshan M 7½ earthquake area and its implications to the Dongzhaigang subsidence, northeastern Hainan Island, China[J]. Journal of Geomechanics，29（3）：339−354 doi: 10.12090/j.issn.1006-6616.20232904
Citation: JIA L Y，MA X M，JING J J，et al.，2023. Dynamic variation characteristics of in-situ stress in the 1605 Qiongshan M 7½ earthquake area and its implications to the Dongzhaigang subsidence, northeastern Hainan Island, China[J]. Journal of Geomechanics，29（3）：339−354 doi: 10.12090/j.issn.1006-6616.20232904
shu

Dynamic variation characteristics of in-situ stress in the 1605 Qiongshan M 7½ earthquake area and its implications to the Dongzhaigang subsidence, northeastern Hainan Island, China

doi: 10.12090/j.issn.1006-6616.20232904
  • 1.

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

  • 2.

    Observation and Research Station of Crustal Stress and Strain in Beijing , Ministry of Natural Resources, Beijing 100081, China

  • 3.

    Key Laboratory of Active Tectonics and Crustal Stability Assessment, Beijing 100081, China

  • 4.

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

  • 5.

    Institute of Geological Survey, China University of Geosciences, Wuhan 430074, Hubei, China

  • 6.

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

Funds:  This research is financially supported by the Geological Survey Projects of the China Geological Survey (Grants DD20230249 and DD20230014), Basic Research Funds of the Institute of Geomechanics, Chinese Academy of Geological Sciences (Grants DZLXS202106 and DZLXJK202211), the National Natural Science Foundation of China (Grant No. 42272222), and the Open Project of the Hainan Key Laboratory of Marine Geological Resources and Environment (Grant 22-HNHYDZZYHJKF022)
More Information
  • Received: 2023-02-28
  • Revised: 2023-04-25
  • Accepted: 2023-05-08
    Abstract

  • Based on the strain data of three in-situ stress monitoring stations in different sections of the 1605 Qiongshan 7½ earthquake area, we studied the dynamic variations of in-situ stress and extracted the sudden stress changes recorded by them. We analyzed the in-situ stress variations and tectonic activity between March 2016 and May 2018 to discuss the geomorphological evolution trends and subsidence mechanisms at the Dongzhai Port. The results show that the study area was generally subjected to the NW-compressive stress field, which makes the tensile stress field dominate in the Yanfeng and Dazhipo areas in the hanging wall of the Maniao-Puqian fault（MPF） and the Puqian-qinglan fault（PQF), while the Jinshan area in the footwall of the faults by compressive stress. The MPF fault and the PQF fault have been constantly engaged in non-seismic activities to adjust the local stress field under the regional stress field, among which the MPF Fault had several activities in March–July 2016, October 2017, and April 2018, and the PQF fault had two activities in October 2017. The energy of the MPF activities is more intensive than that of the PQF. The variation trend of the stress field indicates a gradual upward trend in the east bounded by the MPF fault (F13-1) and possible continued subsidence in Dongzhaigang in the west. The fault activity trend implies that the subsidence rate in  Yanfeng, the northern part of Dongzhaigang, bounded by the MPF fault (F2-2), should be greater than that in the southern Sanjiang area. In addition, the volume strain monitoring data also reveals traces of magmatic activity in the lower part of the N–S seismic zone of Hainan Island. The comprehensive study concluded that the Dongzhaigang subsidence is mainly controlled by the positive fault activity of the MPF and PQF faults due to the upwelling of deep magma and influenced by the Holocene sea level change and the properties of soft soil depositional strata leading to soft soil flow slip, sand liquefaction, and seawater erosion. We innovatively apply the borehole strain observation technology to explore the evolution law and trend of typical earthquake subsidence landforms in coastal zones, which has essential academic value in the fields of in-situ stress monitoring and tectonic geomorphology research, and the results also have significant application value for mangrove protection and urban planning and construction in Dongzhaigang area.

     

    • FullText(HTML)
  • loading
    • References(89)
  • [1]
    CHEN E M, HUANG Y Y, 1979. Preliminary Discussion on the 1605 Qiongzhou earthquake and its Seismogentic Structure. [J]. Seismology and Geology, , 04: 37-44.
    [2]
    CHEN E M, HUANG Y Y, 1989. Earthquake damage characteristics and three-dimensional photoelastic experiments of the 1605 Qiongzhou earthquake in Hainan Island[J]. Journal of Earthquake Engineering(2): 65-72. (in Chinese with English abstract)
    [3]
    CHEN H X, HONG H J, LIU H, 2009. Volcano-tectonic interaction and the relation with the state of volcanic activity[J]. Chinese Journal of Geophysics, 52(5): 1263-1269. (in Chinese with English abstract)
    [4]
    DING Y Y, ZHAO X T, HU D G, et al. , 2018. Late Cenozoic Fault activity in northeastern Hainan Island and its controlling effect on tectonic subsidence in Dongzhai port[J]. Acta Geoscientica Sinica, 39(2): 155-166. (in Chinese with English abstract)
    [5]
    HU D G, MA X M, JIA L Y, et al. , 2019. Report on investigation of active faults in Pan-Pearl River Delta region and evaluation of demineralization and crustal stability[R]. Institute of Geomechanics, Chinese Academy of Geological Sciences. (in Chinese)
    [6]
    HU D G, HAN J E, ZHANG L, et al. , 2022. Report on investigation and evaluation results of active faults and crustal stability in Hainan Island and offshore areas[R]. Institute of Geomechanics, Chinese Academy of Geological Sciences. (in Chinese)
    [7]
    HU J C, BAI D H, WANG W H, et al. , 2007. Magnetotelluric surveying and electrical structure of the deep underground part in Leiqiong volcanic area[J]. South China Journal of Seismology, 27(1): 1-7. (in Chinese with English abstract)
    [8]
    HUANG Z G, CAI F X, HAN Z Y, et al. , 1993. Leiqiong Quaternary volcano[M]. Beijing: Science Press. (in Chinese)
    [9]
    JIA L Y, HU D G, ZHANG L, et al. , 2021-12-17. The past and present lives of Hainan Dongzhai port[N]. China Mining News. (in Chinese)
    [10]
    JIANG J X, YIN G H, XU F Z, 2003. Relative stress field change of Ku'erle region before 8.1 earthquake in western Kunlun Pass[J]. Earthquake, 23(3): 89-96. (in Chinese with English abstract)
    [11]
    LI P, YANG M, LIU X, et al. , 1988. Analysis of active fault in the northern Qiongzhou( A. ). . Ding Yuanzhang. Collection of Earthquake Studies in Northern Hainan Island. Beijing: Seismological Press, 41~52 (in Chinese) .
    [12]
    LI F Q, 1985. In-situ stress measurement[J]. Chinese Journal of Rock Mechanics and Engineering, 4(1): 95-111. (in Chinese )
    [13]
    LI W, JIA L Y, HU D G, et al. , 2019. Late Pleistocene tectonic history of the western segment of Maniao-Puqian fault: evidence from the Laocheng section, northern Hainan Island[J]. Geoscience, 33(5): 970-978. (in Chinese with English abstract)
    [14]
    LIANG D Y, XU G Q, XIAO Y, et al., 2021. Neogene-Quaternary stratigraphic standard and combined zoning of Haikou Jiangdong New District[J]. Science Technology and Engineering, 21(26): 11052-11063.(in Chinese with English abstract)
    [15]
    LIU H G, WU X J, LI F, et al. , 2018. Active characteristics of the middle segment of Maniao-Puqian fault in the Holocene[J]. Technology for Earthquake Disaster Prevention, 13(3): 588-599. (in Chinese with English abstract)
    [16]
    LIU Y, DU J S, HU Z W, et al. , 2021. Crustal magma plumbing system beneath the Quaternary volcanic area (northern Hainan Island, China) revealed by magnetotelluric data[J]. Journal of Volcanology and Geothermal Research, 419: 107362. doi: 10.1016/j.jvolgeores.2021.107362
    [17]
    MENG Q, GAO K, CHEN Q, et al. , 2021. Seismogenic, coseismic and postseismic deformation and stress evolution of the 2008 Wenchuan earthquake: numerical simulation analysis[J]. Journal of Geomechanics, 27(4): 614-627. (in Chinese with English abstract)
    [18]
    PENG C G. 1983. Cause of the Land Subsidence Associated With the Historical Qiong Zhou Earth Quake (13 July 1605)[J]. Seismology and Geology, 5(3), 9-15. (in Chinese with English abstract)
    [19]
    PENG H, MA X M, JIANG J J, 2008. Analysis of the volume strain data from the Shandan in-situ stress monitoring station[J]. Journal of Geomechanics, 14(2): 97-108. (in Chinese with English abstract)
    [20]
    PENG H, MA X M, JIANG J J, 2011. In-situ stress measurement by differential strain analysis method in WFSD-1[J]. Journal of Geomechanics, 17(3): 249-261. (in Chinese with English abstract)
    [21]
    PENG H, MA X M, LI Z. etal. 2019. Report on Geostress Observation and Crustal Stability Evaluation in Bohai Strait, Taiwan Strait, Qiongzhou Strait and Other Sea Areas (Open Edition)[R]. Institute of Geomechanics, Chinese Academy of Geological Sciences. (in Chinese with English abstract)
    [22]
    PENG H, WU Z H, MA X M, 2006. Unmanned in-situ stress monitoring stations along the Qinghai-Tibet railway[J]. Journal of Geomechanics, 12(1): 96-104. (in Chinese with English abstract)
    [23]
    QIN X H, CHEN Q C, MENG W, et al. , 2018. Evaluating measured in-situ stress state changes associated with earthquakes and its implications: a case study in the Longmenshan fault zone[J]. Journal of Geomechanics, 24(3): 309-320. (in Chinese with English abstract)
    [24]
    QIU H, 2004. Research of distribution feature of strain field and evolution of surface rupture caused by earthquake fault[D]. Tianjin: Tianjin University. (in Chinese with English abstract)
    [25]
    QIU Z H, XIE F R, SU K Z, et al. , 2004. New era of borehole strain observation[J]. Recent Developments in World Seismology(1): 7-14. (in Chinese with English abstract)
    [26]
    QIU Z H, KAN B X, TANG L, et al. , 2006. Inversion of coseismic stress-triggered fault slips using borehole strain meter observations[J]. Acta Seismologica Sinica, 28(6): 596-602. (in Chinese with English abstract)
    [27]
    QIU Z H, 2010. A review of component borehole observation of stress-strain in China[J]. Journal of Geodesy and Geodynamics, 30(5): 42-47. (in Chinese with English abstract)
    [28]
    QIU Z H, TANG L, GUO Y P, et al. , 2020. Observing tectonic strain rates using four-gauge-borehole-strainmeters (FGBS)[J]. Progress in Geophysics, 35(5): 1688-1701. (in Chinese with English abstract)
    [29]
    TAN C X, ZHANG P, LU S L, et al. , 2019. Significance and role of in-situ crustal stress measuring and real-time monitoring in earthquake prediction research[J]. Journal of Geomechanics, 25(5): 866-876. (in Chinese with English abstract)
    [30]
    WANG C Q, JIA L Y, HU D G, et al. , 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. (in Chinese with English abstract)
    [31]
    WANG C Q, JIA L Y, HU D G, et al. , 2021. Seismogenic structure of the 1605 Qiongzhou M1/2 earthquake and its Holocene activity history in northern Hainan Island, China: evidence from cross-section drilling and shallow seismic profile[J/OL]. Journal of Earth Sciences: https://kns.cnki.net/kcms/detail/42.1788.P.20211126.1558.004.html.
    [32]
    WANG C Q, JIA L Y, HU D G, et al. , 2022. Quaternary activity characteristics of the Maniao-Puqian fault in the Jiangdong New District of Haikou[J]. Acta Geologica Sinica, 96(2): 403-417. (in Chinese with English abstract)
    [33]
    WANG L M, CHEN C, LIU J P, et al. , 2023. On comprehensive application of seismic reflection and MASW method for investigation of urban subsurface active faults and underneath structures: a case study in Haikou City of Hainan Province, China[J]. Journal of Applied Geophysics, 212: 104982. doi: 10.1016/j.jappgeo.2023.104982
    [34]
    WEST M, SÁNCHEZ J J, MCNUTT S R, 2005. Periodically triggered seismicity at Mount Wrangell, Alaska, after the Sumatra earthquake[J]. Science, 308(5725): 1144-1146. doi: 10.1126/science.1112462
    [35]
    WU G H, 2008. Physical geography[M]. 4th ed. Beijing: Higher Education Press. (in Chinese)
    [36]
    XU Q H, 1985. Discussion on subsidence mechanism of Qiongshan earthquake[J]. South China Journal of Seismology, 5(4): 30-37. (in Chinese)
    [37]
    XU Q H, 1986a. Recent sinking in the Dongzhai Harbour area, northern Qiongzhou[J]. Marine Sciences, 10(1): 24-28. (in Chinese with English abstract)
    [38]
    XU Q H, 1986b. Understanding of seismic geology in Leiqiong Sag[J]. South China Journal of Seismology, 6(1): 83-93. (in Chinese)
    [39]
    XU Q H, 1986c. Formation and migration of Dongzhai port in the Northern Hainan Island and the major Qiongzhou earthquake of 1605[J]. Seismology and Geology, 8(3): 92-96. (in Chinese with English abstract)
    [40]
    XU Q H, 1988. New genesis of Dongzhai Harbor in Hainan Island[J]. Earth(4): 10-11. (in Chinese)
    [41]
    XU Q H, 1990. Subsidence caused by the Qiongzhou large earthquake in 1605 and the formation and vicissitude of Dongzhaigang Bay on Hainan Island[J]. Earthquake Research in China, 4(1): 71-82.
    [42]
    XU Q H, . 2006. The Coseismic Coast Fast Sinkage and the Following Possible Tsunami Caused by the 1605Qiongshan Strong Earthquake and the Evidence[J]. South China Journal of Seismology, 01: 17-27. (in Chinese with English abstract)
    [43]
    XU S C, GAO X K, LI H Y, 1982. Large-scale subsidence may be the evidence of phase transition in the source area: preliminary study on the genesis of the Qiongzhou earthquake[J]. South China Journal of Seismology, 2(1): 3-7. (in Chinese)
    [44]
    XIN P, WANG T, LIU J. , et al. , 2023. The geological structure and sliding model of slope in the triggering area of Yigong landslide in Tibet [J]. Journal of Geomechanics, 29(3): 1012-1023. (in Chinese with English abstract)
    [45]
    YAN Y D, CHEN E M, HUANG Y Y, 1988. Three—dimensional Photoelastic simulating experiments to tectonic stress field of great Qiongzhou earthquake Of 1605 in Hainan, China[J]. Northwestern Seismological Journal, 10(2): 63-70. (in Chinese with English abstract)
    [46]
    YANG J C, LI Y L, 2005. Principles of geomorphology[M]. Beijing: Peking University Press. (in Chinese)
    [47]
    ZHU H, 2008. Using borehole strain data to forecast the Yanjin M5.1 earthquake, Yunnan Province, on 22 July 2006[J]. Earthquake Research in Sichuan(1): 4-8. (in Chinese with English abstract)
    [48]
    陈恩民, 黄咏茵. 1979. 1605年海南岛琼州大地震及其发震构造的初步探讨[J]. 地震地质, 04: 37-44.
    [49]
    陈恩民, 黄咏茵, 1989. 1605 年海南岛琼州大地震的震害特征和发震构造研究. 地震学报, 11(3): 319 - 331.
    [50]
    陈会仙, 洪汉净, 刘辉, 2009. 岩浆活动与构造应力的相互作用及其与火山活动状态的关系[J]. 地球物理学报, 52(5): 1263-1269. doi: 10.3969/j.issn.0001-5733.2009.05.015
    [51]
    丁莹莹, 赵希涛, 胡道功, 等, 2018. 琼东北晚新生代断裂活动及其对东寨港沉降的控制作用[J]. 地球学报, 39(2): 155-166. doi: 10.3975/cagsb.2017.112601
    [52]
    胡道功, 马秀敏, 贾丽云, 等, 2019. 泛珠三角地区活动断裂调查与去与地壳稳定性评价成果报告[R]. 中国地质科学院地质力学研究所.
    [53]
    胡道功, 韩建恩, 张磊, 等, 2022. 海南岛及近海活动断裂与地壳稳定性调查评价成果报告[R]. 中国地质科学院地质力学研究所.
    [54]
    胡久常, 白登海, 王薇华, 等, 2007. 雷琼火山区地下深部大地电磁探测与电性结构分析[J]. 华南地震, 27(1): 1-7. doi: 10.3969/j.issn.1001-8662.2007.01.001
    [55]
    黄镇国, 蔡福祥, 韩中元, 等, 1993. 雷琼第四纪火山[M]. 北京: 科学出版社.
    [56]
    贾丽云, 胡道功, 张磊, 等, 2021-12-17. 海南岛东寨港的前世今生[N]. 第A3版, 地质调查, 中国矿业报.
    [57]
    蒋靖祥, 尹光华, 许凤柱, 2003. 昆仑山口西8.1级地震前库尔勒测区相对应力场变化[J]. 地震, 23(3): 89-96. doi: 10.3969/j.issn.1000-3274.2003.03.012
    [58]
    李方全, 1985. 地应力测量[J]. 岩石力学与工程学报, 4(1): 95-111.
    [59]
    李玶, 杨美娥, 刘行松等. 1988. 琼北地区活动性断裂的研究[A]. 丁原章主编. 海南岛北部地震研究文集. 北京: 地震出版社, 41 - 52.
    [60]
    李薇, 贾丽云, 胡道功, 等, 2019. 琼北老城剖面记录的马袅-铺前断裂西段晚更新世活动历史[J]. 现代地质, 33(5): 970-978.
    [61]
    梁定勇, 许国强, 肖瑶, 等. 2021. 海口江东新区新近纪-第四纪标准地层与组合分区[J]. 科学技术与工程,21(26): 11052-11063.
    [62]
    刘华国, 吴小江, 李峰, 等, 2018. 马袅-铺前断裂中段全新世活动特征研究[J]. 震灾防御技术, 13(3): 588-599.
    [63]
    孟秋, 高宽, 陈启志, 等, 2021. 2008年汶川大地震孕震、同震及震后变形和应力演化全过程的数值模拟[J]. 地质力学学报, 27(4): 614-627.
    [64]
    彭华, 吴珍汉, 马秀敏, 2006. 青藏铁路无人值守地应力综合监测站[J]. 地质力学学报, 12(1): 96-104.
    [65]
    彭华, 马秀敏, 姜景捷, 2008. 山丹地应力监测站体应变仪的地震效应[J]. 地质力学学报, 14(2): 97-108.
    [66]
    彭华, 马秀敏, 姜景捷, 2011. 差应变法地应力测量: 以汶川地震断裂带科学钻探WFSD-1钻孔为例[J]. 地质力学学报, 17(3): 249-261.
    [67]
    彭华, 马秀敏, 李振等. 2019. 渤海海峡、台湾海峡、琼州海峡等海域地应力观测与地壳稳定性评价成果报告(公开版)[R]. 中国地质科学院地质力学研究所.
    [68]
    秦向辉, 陈群策, 孟文, 等, 2018. 大地震前后实测地应力状态变化及其意义: 以龙门山断裂带为例[J]. 地质力学学报, 24(3): 309-320.
    [69]
    邱虎, 2004. 地震断层错动产生的应变场特征的研究及地表破裂的评价[D]. 天津: 天津大学.
    [70]
    邱泽华, 谢富仁, 苏恺之, 等, 2004. 发展钻孔应变观测的战略构想[J]. 国际地震动态(1): 7-14.
    [71]
    邱泽华, 阚宝祥, 唐磊, 等, 2006. 用钻孔应变资料反演同震应力触发断层活动[J]. 地震学报, 28(6): 596-602.
    [72]
    邱泽华, 2010. 中国分量钻孔地应力-应变观测发展重要事件回顾[J]. 大地测量与地球动力学, 30(5): 42-47.
    [73]
    邱泽华, 唐磊, 郭燕平, 等, 2020. 用四分量钻孔应变仪观测构造应变速率[J]. 地球物理学进展, 35(5): 1688-1701.
    [74]
    谭成轩, 张鹏, 路士龙, 等, 2019. 原位地应力测量与实时监测在地震预报研究中的作用和意义[J]. 地质力学学报, 25(5): 866-876.
    [75]
    王超群, 贾丽云, 胡道功, 等, 2021. 海南岛北部马袅-铺前断裂 东段活动性与地壳稳定性评价[J]. 中国地质, 48(2): 618-631.
    [76]
    王超群, 贾丽云, 胡道功, 等, 2022. 海口市江东新区马袅-铺前断裂第四纪活动特征[J]. 地质学报, 96(2): 403-417.
    [77]
    伍光和, 2008. 自然地理学[M]. 4版. 北京: 高等教育出版社.
    [78]
    徐起浩, 1985. 琼山大震沉陷机理讨论[J]. 华南地震, 5(4): 30-37. doi: 10.13512/j.hndz.1985.04.004
    [79]
    徐起浩, 1986a. 琼北东寨港地区的近期下沉[J]. 海洋科学, 10(1): 24-28.
    [80]
    徐起浩, 1986b. 对雷琼凹陷地震地质的认识[J]. 华南地震, 6(1): 83-93.
    [81]
    徐起浩, 1986c. 海南岛北部东寨港的形成、变迁与1605年琼州大地震[J]. 地震地质, 8(3): 92-96.
    [82]
    徐起浩, 1988. 海南岛东寨港成因新说[J]. 地球(4): 10-11.
    [83]
    徐起浩. 2006. 1605年琼山强地震导致的同震海岸快速下沉、可能紧随的海啸及其证据[J]. 华南地震, 01: 17-27.
    [84]
    许寿椿, 高喜奎, 李海玉, 1982. 大面积沉陷可能是震源区相变的证据: 琼州大震成因初探[J]. 华南地震, 2(1): 1-5.
    [85]
    辛鹏, 王涛, 刘甲美, 等, 2023. 西藏易贡滑坡源区坡体赋存的地质结构及其滑动模式[J]. 地质力学学报, 29(3): 1012-1023.
    [86]
    颜玉定, 陈恩民, 黄咏茵, 1988. 1605年琼州大地震构造应力场的三维光弹实验[J]. 西北地震学报, 10(2): 63-70.
    [87]
    杨景春, 李有利, 2005. 地貌学原理[M]. 北京: 北京大学出版社.
    [88]
    朱航, 2008. 使用钻孔应变测值预测2006年7月22日云南盐津5.1级地震[J]. 四川地震(1): 4-8.
    [89]
    彭承光. 1983. 1605年7月13日琼州历史地震陆沉原因[J]. 地震地质, 5(3), 9-15.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    Figures(7)  / Tables(2)

    Get Citation
    PDF
    XML

    Article Metrics

    Article views (1088) PDF downloads(79) Cited by()
    Proportional views
    Related

    Website Copyright © Journal of Geomechanics  京ICP备18031784号  Total visits：

    Supported by: Beijing Renhe Information Technology Co., Ltd.    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return