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Characteristics of Surface Rupture Zone of 1679 Sanhe-Pinggu M 8 Earthquake in Xiadian Fault of Beijing Plain, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2023年第05期
Page:
1257-1269
Research Field:
庆贺汤中立院士从事地质工作七十周年专辑
Publishing date:

Info

Title:
Characteristics of Surface Rupture Zone of 1679 Sanhe-Pinggu M 8 Earthquake in Xiadian Fault of Beijing Plain, China
Author(s):
XING Xiao-qin1; 2; 3;  QI Bang-shen2; 3*;  FENG Cheng-jun2; 3;  YANG Xiao-xiao2; 3;  TAN Cheng-xuan2; 3;  DENG Ya-hong1;  SONG Yan-xun1;  MU Huan-dong4
(1. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 3. Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China; 4. School of Civil Engineering and Architecture, Xi'an University of Technology, Xi'an 710048, Shaanxi, China)
Keywords:
paleoearthquake;  Xiadian fault;  Sanhe-Pinggu earthquake;  surface rupture zone;  violent earthquake;  trench;  formation dislocation;  Beijing
PACS:
P316
DOI:
10.19814/j.jese.2022.12077
Abstract:
The Xiadian fault is one of the most important active faults in Beijing. The Sanhe-Pinggu M 8 earthquake, which occurs on the fault in 1679, is the largest earthquake on record in Beijing and its adjacent areas. The surface forms a seismic surface rupture zone that is still clearly visible. The characteristics of the ancient seismic activity and surface rupture zone of the fault are important for optimizing the land-space development pattern and the disaster prevention and mitigation system in Beijing. Through trench excavation, optically stimulated luminescence(OSL)dating, fault scarp morphology and stratigraphic dislocation analysis, the paleoseismic activity, paleoseismic sequence, and surface rupture zone characteristics of Xiadian fault were revealed. The results show that ① the stratigraphic dislocations, seismic wedges, and colluvial wedges displayed by Dahuzhuang south trench of Xiadian fault reveal two paleoseismic events, which are about(1.610±0.130)ka B.P. and 1679 Sanhe-Pinggu M 8 earthquake; the stratigraphic dislocations are about 0.3 and 2.5 m, respectively; ② there has been seven periods of paleoearthquake events since 20 ka on Xiadian fault, and the average recurrence period of violent earthquakes is about 2 716 years; ③ however, in the Dakangzhuang-Qixinzhuang sections, the stratigraphic dislocation distance is greater than the height of the fault scarp measured on the ground, indicating that the surface fault scarp morphology may be affected by human activities. The amount of stratigraphic dislocation revealed by the trench is helpful to further understand the surface rupture zone characteristics of 1679 Sanhe-Pinggu M 8 earthquake on Xiadian fault.

References:

[1] ZHOU C D,LAN H X,BURGMANN R,et al.Application of an Improved Multi-temporal InSAR Method and Forward Geophysical Model to Document Subsidence and Rebound of the Chinese Loess Plateau Following Land Reclamation in the Yan'an New District[J].Remote Sensing of Environment,2022,279:113102.
[2] LAN H X,MARTIN C D,ZHOU C H,et al.Rockfall Hazard Analysis Using LiDAR and Spatial Modeling[J].Geomorphology,2010,118(1/2):213-223.
[3] LAN H X,MARTIN C D,LIM C H.Rockfall Analyst:A GIS Extension for Three-dimensional and Spatially Distributed Rockfall Hazard Modeling[J].Computers & Geosciences,2007,33(2):262-279.
[4] 刘世杰,兰恒星,张 宁.嘉黎断裂中段重大工程区地质力学分析[J].工程地质学报,2022,30(6):1947-1961.
LIU Shi-jie,LAN Heng-xing,ZHANG Ning.Geomechanical Analysis of Major Engineering Region in Mi-ddle Segment of Jiali Fault[J].Journal of Engineering Geology,2022,30(6):1947-1961.
[5] LI L P,LAN H X,GUO C B,et al.A Modified Frequency Ratio Method for Landslide Susceptibility Assessment[J].Landslides,2017,14(2):727-741.
[6] YAO J M,LAN H X,LI L P,et al.Characteristics of a Rapid Landsliding Area Along Jinsha River Revealed by Multi-temporal Remote Sensing and Its Risks to Sichuan-Tibet Railway[J].Landslides,2022,19(3):703-718.
[7] LAN H X,ZHOU C H,WANG L J,et al.Landslide Hazard Spatial Analysis and Prediction Using GIS in the Xiaojiang Watershed,Yunnan,China[J].Engineering Geology,2004,76(1/2):109-128.
[8] 徐锡伟,计凤桔,于贵华,等.用钻孔地层剖面记录恢复古地震序列:河北夏垫断裂古地震研究[J].地震地质,2000,22(1):9-19.
XU Xi-wei,JI Feng-ju,YU Gui-hua,et al.Reconstruc-tion of Paleoearthouake Sequence Using Stratigraphic Records from Drill Logs:A Study at the Xiadian Fault,Hebei[J].Seismology and Geology,2000,22(1):9-19.
[9] 雷晓东,戚帮申,关 伟,等.北京平原区断裂构造重力异常识别研究[J].地球物理学报,2021,64(4):1253-1265.
LEI Xiao-dong,QI Bang-shen,GUAN Wei,et al.Research on the Faults Identification Based on Gravity Anomaly in Beijing Plain[J].Chinese Journal of Geophysics,2021,64(4):1253-1265.
[10] 马振宁,钱荣毅,CATCHINGS R,等.美国南加州Ri-dgecrest Mw 6.4～Mw 7.1地震地表破裂几何学及运动学特征[J].地球物理学报,2021,64(4):1206-1214.
MA Zhen-ning,QIAN Rong-yi,CATCHINGS R,et al.Geometric and Kinematic Characteristics of Surface Ruptures of Ridgecrest Mw 6.4-Mw 7.1 Earthquake in Southern California[J].Chinese Journal of Geophy-sics,2021,64(4):1206-1214.
[11] 冉勇康,邓起东,杨晓平,等.1679年三河—平谷8级地震发震断层的古地震及其重复间隔[J].地震地质,1997,19(3):2-10.
RAN Yong-kang,DENG Qi-dong,YANG Xiao-ping,et al.Paleoearthquakes and Recurrence Interval on the Seismogenic Fault of 1679 Sanhe-Pinggu M 8 Earthquake,Hebei and Beijing[J].Seismology and Geology,1997,19(3):2-10.
[12] 孟宪梁,杜春涛,王 瑞,等.1679年三河—平谷大震的地震断裂带[J].地震,1983(3):18-23.
MENG Xian-liang,DU Chun-tao,WANG Rui,et al.The Seismic Fault Zone of the 1679 Sanhe-Pinggu Earthquake[J].Earthquake,1983(3):18-23.
[13] 计凤桔,冉勇康,李建平,等.东柳河屯探槽沉积物的热释光测年及其地质意义[J].核技术,1997(8):50-53.
JI Feng-ju,RAN Yong-kang,LI Jian-ping,et al.The TL Dating of Sediments in Dongliuhetun Trench and Its Geological Significance[J].Nuclear Techniques,1997(8):50-53.
[14] 毛昌伟,丁 锐,龚 正,等.1679年三河—平谷8级地震地表断层陡坎的GPS测量[J].地壳构造与地壳应力文集,2010(1):11-18.
MAO Chang-wei,DING Rui,GONG Zheng,et al.GPS Survey of the Surface Fault Scarp of 1679 Sanhe-Pinggu M 8 Earthquake[J].Bulletin of the Institute of Crustal Dynamics,2010(1):11-18.
[15] YU Z Y,PAN H,XI H,et al.Late Quaternary Paleoseismicity of the Xiadian Fault in the North China Plain with Implications for Earthquake Potential[J].Journal of Asian Earth Sciences,2019,184:103997.
[16] 向宏发,方仲景,张晚霞,等.北京平原区隐伏断裂晚第四纪活动性的初步研究[J].地震学报,1993(3):385-388,400.
XIANG Hong-fa,FANG Zhong-jing,ZHANG Wan-xia,et al.A Preliminary Study on Late Quarternary Activity of Hidden Faults in Beijing Plain Area[J].Acta Seismologica Sinica,1993(3):385-388,400.
[17] 李占飞,徐锡伟,孟勇琦,等.基于“吉林一号”高精度遥感数据研究华北地区最新构造变形样式:以夏垫断裂1679年三河—平谷地震地表破裂为例[J].地震地质,2022,44(1):98-114.
LI Zhan-fei,XU Xi-wei,MENG Yong-qi,et al.The Latest Deformation Style Along the North China Block Revealed by High-resolution Topographic Data:A Case Study on Xiadian Fault[J].Seismology and Geology,2022,44(1):98-114.
[18] 邓 梅,沈 军,李 西,等.夏垫断裂大胡庄探槽古地震事件分析[J].地震研究,2018,41(2):293-301,344.
DENG Mei,SHEN Jun,LI Xi,et al.Analysis of Paleoseismic Events of the Dahuzhuang Trench at the Xiadian Fault[J].Journal of Seismological Research,2018,41(2):293-301,344.
[19] 高战武,陈棋福,黄金莉,等.北京地区主要活动断裂深部速度结构特征及强震构造分析[J].震灾防御技术,2010,5(3):271-280.
GAO Zhan-wu,CHEN Qi-fu,HUANG Jin-li,et al.Velocity Structure Beneath the Active Faults in Beijing Area and Their Seismotectonic Characteristics[J].Technology for Earthquake Disaster Prevention,2010,5(3):271-280.
[20] 江娃利,侯治华,肖振敏,等.北京平原夏垫断裂齐心庄探槽古地震事件分析[J].地震地质,2000,22(4):413-422.
JIANG Wa-li,HOU Zhi-hua,XIAO Zhen-min,et al.Study on Paleoearthquakes of Qixinzhuang Trench at the Xiadian Fault,Beijing Plain[J].Seismology and Geology,2000,22(4):413-422.
[21] 徐 杰,高战武,宋长青,等.太行山山前断裂带的构造特征[J].地震地质,2000(2):111-122.
XU Jie,GAO Zhan-wu,SONG Chang-qing,et al.The Structural Characters of the Piedmont Fault Zone of Taihang Mountain[J].Seismology and Geology,2000(2):111-122.
[22] 汪良谋,徐 杰,黄秀铭,等.北京拗陷构造活动性分析[J].中国地震,1990,6(2):25-36.
WANG Liang-mou,XU Jie,HUANG Xiu-ming,et al.Analysis of Tectonic Activity in Beijing Depression[J].Earthquake Research in China,1990,6(2):25-36.
[23] 戚帮申,潘智锋,丰成君,等.北京顺义断裂第四纪活动性地球物理及钻孔综合探测证据[J].地质学报,2020,94(4):1315-1329.
QI Bang-shen,PAN Zhi-feng,FENG Cheng-jun,et al.Application of Comprehensive Geophysical-drilling Exploration to Detect the Buried Shunyi Active Fault Belt in Beijing[J].Acta Geologica Sinica,2020,94(4):1315-1329.
[24] 张 磊,何 静,白凌燕,等.北京凹陷北缘第四纪凹陷盆地沉积速率变化特征与顺义断裂活动性的响应关系[J].中国地质,2016,43(2):511-519.
ZHANG Lei,HE Jing,BAI Ling-yan,et al.The Response Relationship Between the Variation Characte-ristics of Deposition Rate of Quaternary Depression Basin on the Northern Margin of Beijing Depression and the Activity of Shunyi Fault[J].Geology in China,2016,43(2):511-519.
[25] 赵成彬,刘保金,姬计法,等.北京南部地壳精细结构深地震反射探测研究[J].地球物理学报,2013,56(4):1168-1176.
ZHAO Cheng-bin,LIU Bao-jin,JI Ji-fa,et al.Fine Crustal Structure in the South of Beijing Revealed by Deep Seismic Reflection Profiling[J].Chinese Journal of Geophysics,2013,56(4):1168-1176.
[26] 姜大伟.龙门山南段及其前陆区晚第四纪构造变形的河流地貌研究[D].北京:中国地震局地质研究所,2017.
JIANG Da-wei.A Fluvial Geomorphology Research About the Late Quaternary Deformation of the Southern Longmen Shan and Its Foreland Basin[D].Beijing:Institute of Geology,China Earthquake Administration,2017.
[27] 张培震,闵 伟,邓起东,等.海原活动断裂带的古地震与强震复发规律[J].中国科学:D辑,地球科学,2003,33(8):705-713.
ZHANG Pei-zhen,MIN Wei,DENG Qi-dong,et al.Paleoearthquake Rupture Behavior and Recurrence of Great Earthquakes Along the Haiyuan Fault,Northwestern China[J].Science in China:Series D,Earth Sciences,2003,33(8):705-713.
[28] 万永魁,沈 军,于晓辉,等.北京平原区夏垫活动断裂滑动速率及古地震复发间隔[J].防灾科技学院学报,2014,16(3):38-45.
WAN Yong-kui,SHEN Jun,YU Xiao-hui,et al.The Slipping Rates and Ancient Earthquake Recurrence Interval at Xiadian Fault,Beijing Plain[J].Journal of Institute of Disaster Prevention,2014,16(3):38-45.
[29] 江娃利,候治华,苏怡之,等.北京平原主要活动断裂全新世活动定量研究及未来地震危险性预测[J].地壳构造与地壳应力文集,2000(1):1-15.
JIANG Wa-li,HOU Zhi-hua,SU Yi-zhi,et al.Quantitative Study of Holocene Activity of Main Active Faults in the Beijing Plain and Prediction of Future Seismic Danger[J].Bulletin of the Institute of Crustal Dynamics,2000(1):1-15.
[30] 邓起东,刘百篪,张培震,等.活动断裂工程安全评价和位错量的定量评估[M]∥《活动断裂研究》编委会.活动断裂研究:理论与应用,第二辑.北京:地震出版社,1992:236-246.
DENG Qi-dong,LIU Bai-chi,ZHANG Pei-zhen,et al.Safety Evaluation of Active Fault Engineering and Quantitative Evaluation of Dislocation Amount[M]∥Editorial Committee for Active Fault Research.Active Fault Research:Theory and Application,Volume Ⅱ.Beijing:Seismological Press,1992:236-246.
[31] 向宏发,方仲景,徐 杰,等.三河—平谷8级地震区的构造背景与大震重复性研究[J].地震地质,1988,10(1):15-28.
XIANG Hong-fa,FANG Zhong-jing,XU Jie,et al.Study on the Tectonic Background and the Repeatability of Large Earthquakes in the Sanhe-Pinggu Earthquake Region with M 8[J].Seismology and Geo-logy,1988,10(1):15-28.

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Last Update: 2023-10-15