Advanced Search
Zhu Y J，Luo Y，Zhao L. 2023. Rupture process of the 2022 MS6.9 Menyuan，Qinghai earthquake revealed by inversion of regional broadband seismograms. Acta Seismologica Sinica，45（5）：781−796. DOI: 10.11939/jass.20220148
Citation: Zhu Y J，Luo Y，Zhao L. 2023. Rupture process of the 2022 MS6.9 Menyuan，Qinghai earthquake revealed by inversion of regional broadband seismograms. Acta Seismologica Sinica，45（5）：781−796. DOI: 10.11939/jass.20220148
shu

Rupture process of the 2022 MS6.9 Menyuan，Qinghai earthquake revealed by inversion of regional broadband seismograms

  • 1.

    Hebei Hongshan National Observatory on Thick Sediments and Seismic Hazards，Hebei Xingtai 054000，China

  • 2.

    Key Laboratory of Earthquake Prediction，Institute of Earthquake Forecasting，China Earthquake Administration，Beijing 100036，China

  • 3.

    School of Earth and Space Sciences，Peking University，Beijing 100871，China

  • 4.

    Hebei Earthquake Agency，Shijiazhuang 050021，China

  • 5.

    School of Earth and Space Sciences，University of Science and Technology of China，Hefei 230026，China

More Information
  • Received Date: August 15, 2022
  • Revised Date: September 27, 2022
  • Available Online: September 29, 2022
    Graphical Abstract
    • Abstract

  • Finite fault inversion is an effective method commonly used to study the rupture process of earthquakes and has been widely applied to seismic source rupture process research. In this study, we utilized the method to investigate the rupture process of the MS6.9 Menyuan, Qinghai earthquake in 2022 using regional broadband seismic waveform data. Considering the quality and distribution of the network data, we selected 20 regional seismic stations with high signal-to-noise ratio and epicentral distances less than 500 km. We preprocessed the observed waveforms by removing instrument response, demeaning, detrending, and filtering. We also calculated the near-field Green’s functions using the frequency-wavenumber （f-k） method. 　　First, synthesize the waveforms using the Green’s function synthesis theory and compare them with corresponding observed waveforms. Then, perform fault model inversion where the displacement response of each sub-fault at any station can be represented as a function of the sub-fault’s slip, direction, rise time, and rupture velocity. Additionally, in the process of reducing errors, we use wavelet transform to establish the objective function and use simulated annealing （SA） to search for the global optimal solution of each sub-fault parameter, so that the waveform residual can be minimized in the wavelet domain, ultimately obtaining the best spatio-temporal distribution model of the source fault slip. 　　In this study, high frequency signal of regional network is used. Low-frequency information constrains the overall characteristics of the earthquake source, but is less sensitive to detailed rupture features such as rupture rise time or rupture velocity changes. However, sudden changes in slip amplitude or rupture velocity will radiate intense seismic signals with higher-frequency. Therefore, using higher-frequency signals for finite fault inversion can effectively improve spatial and temporal resolution, and fully utilize the wide-band information of seismic waves to better understand the earthquake source rupture process. 　　The following results were obtained: ① The seismic fault is nodal planeⅠ（strike 104.2°, dip 84.6°, rake −5.4°）. The rupture is mainly concentrated in two areas. The first area is a circular region with a radius of approximately 3 km above the hypocenter, with a maximum displacement of about 1.5 m, located at a depth of about 6 km underground, where the depth of obvious rupture is about 16 km. The earthquake caused a rupture to the surface with a maximum displacement of approximately 0.5 m, and the surface rupture length is about 20 km. Second, along the strike direction, the circular area with a radius of about 3 km is at the lower-right of the hypocenter, with a maximum displacement of approximately 1.2 m, at a depth of about 14 km. ② The scalar seismic moment released by the earthquake is 1.23×1019 N·m, corresponding to MW6.7. The earthquake rupture lasts about 17 s, with the maximum release of energy occurring around 8 s. The energy was mostly released before 15 seconds. ③ From the perspective of rupture direction, the rupture mainly propagates along the ESE direction. The maximum rupture values appear on both sides of the epicenter at 2 s and 9 s, reflecting the characteristics of bilateral rupture. According to the surface dislocation distribution map, the dip of the seismic fault surface is 84.6°, which is close to vertical. Therefore, the surface projection with obvious dislocation distribution is as long as 34 km. ④ Two obvious features can be identified: first, the fault plane has a large dip and releases a high amount of energy, resulting in significant surface ruptures with a length of approximately 18 km; second, there is bilateral rupture, accompanied with large displacements observed on both sides of the epicenter at 2 s and 9 s. The regional tectonic position also confirms that the initial rupture occurred along the Tuolaishan fault in an approximate E-W direction and triggered the NW-SE trending Lenglongling fault, which is closely related to the complex tectonic environment in the area.

    • FullText(HTML)
    • References (84)
  • 陈文彬. 2003. 河西走廊及邻近地区最新构造变形基本特征及构造成因分析[D]. 北京: 中国地震局地质研究所: 59–69.
    Chen W B. 2003. Principal Features of Tectonic Deformation and Their Generation Mechanism in the Hexi Corridor and Its Adjacent Regions Since Late Quaternary[D]. Beijing: Institute of Geology, China Earthquake Administration: 59–69 （in Chinese）.
    范莉苹,李珀任,廖诗荣,蒋策,房立华. 2022. 2022 年 1 月 8 日青海门源 MS6.9 地震余震序列精定位研究[J]. 地震学报,35(2):138–145.
    Fan L P,Li B R,Liao S R,Jiang C,Fang L H. 2022. Precise relocation of the aftershock sequences of the 2022 M6.9 Menyuan earthquake[J]. Acta Seismologica Sinica,35(2):138–145 (in Chinese). doi: 10.1016/j.eqs.2022.01.021
    国家地震局地质研究所, 宁夏回族自治区地震局. 1990. 海原活动断裂带[M]. 北京: 地震出版社: 99–138.
    Institute of Geology, State Seismological Bureau, Seismological Bureau of Ningxia Hui Autonomous Region. 1990. Haiyuan Active Fault System[M]. Beijing: Seismological Press: 99–138 （in Chinese）.
    郭鹏,韩竹军,安艳芬,姜文亮,毛泽斌,冯蔚. 2017. 冷龙岭断裂系活动性与2016年门源6.4级地震构造研究[J]. 中国科学:地球科学,47:617–630.
    Guo P,Han Z J,An Y F,Jiang W L,Mao Z B,Feng W. 2017. Activity of the Lenglongling fault system and seismotectonics of the 2016 MS6.4 Menyuan earthquake[J]. Science China Earth Sciences,60:929–942.
    韩帅,吴中海,高扬,卢海峰. 2022. 2022年1月8日青海门源MS6.9地震地表破裂考察的初步结果及对冷龙岭断裂活动行为和区域强震危险性的启示[J]. 地质力学学报,28(2):155–168.
    Han S,Wu Z H,Gao Y,Lu H F. 2022. Surface rupture investigation of the 2022 Menyuan MS6.9 earthquake,Qinghai,China:Implications for the fault behavior of the Lenglongling fault and regional intense earthquake risk[J]. Journal of Geomechanics,28(2):155–168 (in Chinese).
    韩竹军, 牛鹏飞, 李科长, 吕丽星. 2022. 2022年1月8日青海门源6.9级地震的一些初步认识[EB/OL]. [2022-01-18]. https://www.eq-igl.ac.cn/zhxw/info/2022/36632.html.
    Han Z J, Niu P F, Li K Z, Lü L X. 2022. Primary understanding of the MS6.9 Menyuan earthquake on January 8, 2022 in Qinghai Province[EB/OL]. [2022-01-18]. https://www.eq-igl.ac.cn/zhxw/info/2022/36632.html （in Chinese）.
    何文贵,刘百篪,袁道阳,杨明. 2000. 冷龙岭活动断裂的滑动速率研究[J]. 西北地震学报,22(1):90–97.
    He W G,Liu B C,Yuan D Y,Yang M. 2000. Research on slip rates of the Lenglongling active fault zone[J]. Northwestern Seismological Journal,22(1):90–97 (in Chinese).
    何文贵,袁道阳,葛伟鹏,罗浩. 2010. 祁连山活动断裂带中东段冷龙岭断裂滑动速率的精确厘定[J]. 地震,30(1):131–137. doi: 10.3969/j.issn.1000-3274.2010.01.015
    He W G,Yuan D Y,Ge W P,Luo H. 2010. Determination of the slip rate of the Lenglongling fault in the middle and eastern segments of the Qilian mountain active fault zone[J]. Earthquake,30(1):131–137 (in Chinese).
    李祥,万永革,崔华伟,高熹微,黄骥超,张珊珊. 2016. 2016年1月21日青海门源 MS6.4 地震构造应力场[J]. 华北地震科学,34(2):36–41. doi: 10.3969/j.issn.1003-1375.2016.02.007
    Li X,Wan Y G,Cui H W,Gao X W,Huang J C,Zhang S S. 2016. Tectonic stress field of 2016,MS6.4 Menyuan,Qinghai earthquake[J]. North China Earthquake Sciences,34(2):36–41 (in Chinese).
    李振洪,韩炳权,刘振江,张苗苗,余琛,陈博,刘海辉,杜静,张双成,朱武,张勤,彭建兵. 2022. InSAR 数据约束下的 2016 年和 2022 年青海门源地震震源参数及其滑动分布[J]. 武汉大学学报(信息科学版),47(6):887–897.
    Li Z H,Han B Q,Liu Z J,Zhang M M,Yu C,Chen B,Liu H H,Du J,Zhang S C,Zhu W,Zhang Q,Peng J B. 2022. Source parameters and slip distributions of the 2016 and 2022 Menyuan,Qinghai earthquakes constrained by InSAR observations[J]. Geomatics and Information Science of Wuhan University,47(6):887–897 (in Chinese).
    李智敏,盖海龙,李鑫,袁道阳,谢虹,姜文亮,李永生,苏琦. 2022. 2022年青海门源MS6.9级地震发震构造和地表破裂初步调查[J]. 地质学报,96(1):330–335.
    Li Z M,Gai H L,Li X,Yuan D Y,Xie H,Jiang W L,Li Y S,Su Q. 2022. Seismogenic fault and coseismic surface deformation of the Menyuan MS6.9 earthquake in Qinghai,China[J]. Acta Geologica Sinica,96(1):330–335 (in Chinese).
    刘成利,郑勇,葛粲,熊熊,许厚泽. 2013. 2013年芦山7.0级地震的动态破裂过程[J]. 中国科学:地球科学,43(6):1020–1026.
    Liu C L, Zheng Y, Ge C, Xiong X, Xu H Z. 2013. Rupture process of the MS7.0 Lushan earthquake, 2013[J]. Science China Earth Sciences, 56（7）: 1187−1192. doi: 10.1007/s11430-013-4639-9.
    刘成利,郑勇,熊熊,付芮,单斌,刁法启. 2014. 利用区域宽频带数据反演鲁甸MS6.5 级地震震源破裂过程[J]. 地球物理学报,57(9):3028–3037. doi: 10.6038/cjg20140927
    Liu C L,Zheng Y,Xiong X,Fu R,Shan B,Diao F Q. 2014. Rupture process of MS6.5 Ludian earthquake constrained by regional broadband seismograms[J]. Chinese Journal of Geophysics,57(9):3028–3037 (in Chinese).
    刘泽民,张广伟,梁姗姗,邹立晔. 2022. 2022年青海门源 MS6.9地震余震的空间迁移特征[J]. 地震工程学报,44(1):475–487.
    Liu Z M,Zhang G W,Liang S S,Zou L Y. 2022. Spatial migration characteristics of the aftershock sequence of the Menyuan,Qinghai MS6.9 earthquake in 2022[J]. China Earthquake Engineering Journal,44(1):475–487 (in Chinese).
    潘家伟,李海兵,Chevalier M L,刘栋梁,李超,刘富财,吴琼,卢海建,焦利青. 2022. 2022年青海门源MS6.9地震地表破裂带及发震构造研究[J]. 地质学报,96(1):215–231. doi: 10.3969/j.issn.0001-5717.2022.01.018
    Pan J W,Li H B,Chevalier M L,Liu D L,Li C,Liu F C,Wu Q,Lu H J,Jiao L Q. 2022. Coseismic surface rupture and seismogenic structure of the 2022 MS6.9 Menyuan earthquake,Qinghai Province,China[J]. Acta Geologica Sinica,96(1):215–231 (in Chinese).
    石富强,邵志刚,占伟,丁晓光,朱琳,李玉江. 2018. 青藏高原东北缘活动断裂剪切模量及应力状态数值模拟[J]. 地球物理学报,61(9):3651–3663. doi: 10.6038/cjg2018L0631
    Shi F Q,Shao Z G,Zhan W,Ding X G,Zhu L,Li Y J. 2018. Numerical modeling of the shear modulus and stress state of active faults in the northeastern margin of the Tibetan Plateau[J]. Chinese Journal of Geophysics,61(9):3651–3663 (in Chinese).
    徐锡伟,吴熙彦,于贵华,谭锡斌,李康. 2017. 中国大陆高震级地震危险区判定的地震地质学标志及其应用[J]. 地震地质,39(2):219–275.
    Xu X W,Wu X Y,Yu G H,Tan X B,Li K. 2017. Seismo-geological signatures for identifying M≥7.0 earthquake risk areas and their premilimary application in mainland China[J]. Seismology and Geology,39(2):219–275 (in Chinese).
    许英才,郭祥云,冯丽丽. 2022. 2022年1月8日青海门源MS6.9地震序列重定位和震源机制解研究[J]. 地震学报,44(2):195–210.
    Xu Y C,Guo X Y,Feng L L. 2022. Relocation and focal mechanism solutions of the MS6.9 Menyuan earthquake sequence on January 8,2022 in Qinghai Province[J]. Acta Seismologica Sinica,44(2):195–210 (in Chinese).
    袁道阳,张培震,刘百篪,甘卫军,毛凤英,王志才,郑文俊,郭华. 2004. 青藏高原东北缘晚第四纪活动构造的几何图像与构造转换[J]. 地质学报,78(2):270–278. doi: 10.3321/j.issn:0001-5717.2004.02.017
    Yuan D Y,Zhang P Z,Liu B C,Gan W J,Mao F Y,Wang Z C,Zheng W J,Guo H. 2004. Geometrical imagery and tectonic transformation of Late Quaternary active tectonics in northeastern margin of Qinghai-Xizang Plateau[J]. Acta Geologica Sinica,78(2):270–278 (in Chinese).
    张勇,许力生,陈运泰,汪荣江. 2014. 2014年2月12日于田MW6.9地震破裂过程初步反演:兼论震源机制对地震破裂过程反演的影响[J]. 地震学报,36(2):159–164. doi: 10.3969/j.issn.0253-3782.2014.02.001
    Zhang Y,Xu L S,Chen Y T,Wang R J. 2014. Fast inversion for the rupture process of the 12 February 2014 Yutian MW6.9 earthquake:Discussion on the impacts of focal mechanism on rupture process inversions[J]. Acta Seismologica Sinica,36(2):159–164 (in Chinese).
    张勇,陈运泰,许力生,魏星,金明培,张森. 2015. 2014年云南鲁甸MW6.1地震:一次共轭破裂地震[J]. 地球物理学报,58(1):153–162. doi: 10.6038/cjg20150113
    Zhang Y,Chen Y T,Xu L S,Wei X,Jin M P,Zhang S. 2015. The 2014 MW6.1 Ludian,Yunnan,earthquake:A complex conjugated ruptured earthquake[J]. Chinese Journal of Geophysics,58(1):153–162 (in Chinese).
    中国地震局地球物理研究所. 2022. 2022年01月08日青海海北州门源县6.9级地震科技支撑简报[EB/OL]. [2022-01-10]. https://www.cea-igp.ac.cn/kydt/278809.html.
    Institute of Geophysics, China Earthquake Administration. 2022. A brief of the MS6.9 Menyuan earthquake on January 8, 2022 in Qinghai Province[EB/OL]. [2022-01-10]. https://www.cea-igp.ac.cn/kydt/278809.html （in Chinese）.
    中国地震局地质研究所. 2022. 2022年01月08日青海海北州门源县6.9级地震科技支撑简报[EB/OL]. [2022-01-14]. https://www.eq-igl.ac.cn/kydt/info/2022/36614.html.
    Institute of Geology, China Earthquake Administration. 2022. A brief of the MS6.9 Menyuan earthquake on January 8, 2022 in Qinghai Province [EB/OL]. [2022-01-14]. https://www.eq-igl.ac.cn/kydt/info/2022/36614.html （in Chinese）.
    中国地震台网中心. 2022. 青海海北州门源县6.9级地震[EB/OL]. [2022-01-10]. https://news.ceic.ac.cn/CC20220108014528.html.
    China Earthquake Networks Center. 2022. MS6.9 Menyuan earthquake in Haibei Prefecture, Qinghai Province[EB/OL]. [2022-01-10]. https://news.ceic.ac.cn/CC20220108014528.html （in Chinese）.
    钟世军,吴建平,房立华,王未来,范莉苹,王怀富. 2017. 青藏高原东北缘及周边地区基于程函方程的面波层析成像[J]. 地球物理学报,60(6):2304–2314. doi: 10.6038/cjg20170622
    Zhong S J,Wu J P,Fang L H,Wang W L,Fan L P,Wang H F. 2017. Surface wave Eikonal tomography in and around the northeastern margin of the Tibetan Plateau[J]. Chinese Journal of Geophysics,60(6):2304–2314 (in Chinese).
    朱音杰,罗艳,赵里,田建慧. 2022. 利用区域宽频地震数据反演2021年5月云南漾濞MS6.4地震震源破裂过程[J]. 地球物理学报,65(3):1021–1031. doi: 10.6038/cjg2022P0443
    Zhu Y J,Luo Y,Zhao L,Tian J H. 2022. Rupture process of Yunnan Yangbi MS6.4 earthquake constrained by regional broadband seismograms[J]. Chinese Journal of Geophysics,65(3):1021–1031 (in Chinese).
    周琳,季灵运,李长军,李君. 2022. 利用小震和 GPS 资料分析冷龙岭地区现今变形过程与地震活动[J]. 地震研究,45(3):416–423.
    Zhou L, Ji L Y, Li Z J, Li J. 2022. Study on current deformation process and seismicity of Lenglongling area based on small earthquakes and GPS Data[J]. Journal of Seismological Research, 45（3）: 416–423 （in Chinese）.
    左可桢,陈继锋. 2018. 门源地区地壳三维体波速度结构及地震重定位研究[J]. 地球物理学报,61(7):2788–2801. doi: 10.6038/cjg2018L0537
    Zuo K Z,Chen J F. 2018. 3D body-wave velocity structure of crust and relocation of earthquakes in the Menyuan area[J]. Chinese Journal of Geophysics,61(7):2788–2801 (in Chinese).
    Aki K, Richards P G. 1980. Quantitative Seismology: Theory and Methods[M]. San Francisco: W. H. Freeman & Co.: 1−813.
    Burchfiel B C,Hodges K V,Royden L H. 1987. Geology of Panamit Valley-Saline Valley pull-apart system,California:Palinspastic evidence for low-angle geometry of a Neogene range-bounding fault[J]. J Geophys Res:Solid Earth,92(B10):10422–10426.
    England P,Molnar P. 1997. Active deformation of Asia:From kinematics to dynamics[J]. Science,278(5338):647–650. doi: 10.1126/science.278.5338.647
    Gaudemer Y,Tapponnier P,Meyer B,Peltzer G,Guo S M,Chen Z T,Dai H G,Cifuentes I. 1995. Partitioning of crustal slip between linked,active faults in the eastern Qilian Shan,and evidence for a major seismic gap,the ‘Tianzhu gap’,on the western Haiyuan fault,Gansu (China)[J]. Geophys J Int,120(3):599–645.
    Guo P,Han Z J,Dong S,Yuan R M,Xie Z D. 2019a. Surface rupture and slip distribution along the Lenglongling fault in the NE Tibetan Plateau:Implications for faulting behavior[J]. J Asian Earth Sci,172:190–207. doi: 10.1016/j.jseaes.2018.09.008
    Guo P,Han Z J,Mao Z B,Xie Z D,Dong S P,Gao F,Gai H L. 2019b. Paleoearthquakes and rupture behavior of the Lenglongling fault:Implications for seismic hazards of the northeastern margin of the Tibetan Plateau[J]. J Geophys Res:Solid Earth,124(2):1520–1543. doi: 10.1029/2018JB016586
    Guo P,Han Z J,Gao F,Zhu C H,Gai H L. 2020. A new tectonic model for the 1927 M8.0 Gulang earthquake on the NE Tibetan Plateau[J]. Tectonics,39(9):e2020TC006064.
    Han S C,Zhang H J,Xin H L,Shen W S,Yao H J. 2022. USTClitho2.0:Updated unified seismic tomography models for continental China lithosphere from joint inversion of body-wave arrival times and surface-wave dispersion data[J]. Seismol Res Lett,93(1):201–205.
    Hsieh M C,Zhao L,Ji C,Ma K F. 2016. Efficient inversions for earthquake slip distributions in 3D structures[J]. Seismol Res Lett,87(6):1342–1354. doi: 10.1785/0220160050
    Ji C, Wald D J, Helmberger D V. 2002. Source description of the 1999 Hector Mine, California, earthquake, part I: Wavelet domain inversion theory and resolution analysis[J], Bull Seismol Soc Am, 92（4）: 1192–1207.
    Ji C, Helmberger D V, Wald D J, Ma K F. 2003. Slip history and dynamic implications of the 1999 Chi-Chi, Taiwan, earthquake[J]. J Geophys Res: Solid Earth, 108（B9）: 2412.
    Lasserre C,Gaudemer Y,Tapponnier P,Mériaux A S,Yuan D Y,Ryerson F J,Finkel R C,Caffee M W. 2002. Fast Late Pleistocene slip rate on the Leng Long Ling segment of the Haiyuan fault,Qinghai,China[J]. J Geophys Res:Solid Earth,107(B11):2276.
    Molnar P,Tapponnier P. 1975. Cenozoic tectonics of Asia:Effects of a continental collision[J]. Science,189(4201):419–426. doi: 10.1126/science.189.4201.419
    Replumaz A,Tapponnier P. 2003. Reconstruction of the deformed collision zone between India and Asia by backward motion of lithospheric blocks[J]. J Geophys Res:Solid Earth,108(B6):2285.
    Royden L,Burchfiel B C,King R W,Wang E,Chen Z,Shen F,Liu Y. 1997. Surface deforlations of a population of very small rift-related normal faults[J]. Geology,24:683–686.
    Shao G,Li X Y,Ji C. 2011. Focal mechanism and slip history of the 2011 MW9.1 of the Pacific coast of Tohoku earthquake,constrained with teleseismic body and surface waves[J]. Earth Planets Space,63(7):559–564. doi: 10.5047/eps.2011.06.028
    Tapponnier P, Molnar P. 1977. Active faulting and tectonics in China[J]. J Geophys Res: Solid Earth, 82: 2905–2930.
    Tapponnier P,Meyer B,Avouac J P,Peltzer G,Gaudemer Y,Guo S M,Xiang H F,Yin K L,Chen Z T,Cai S H,Dai H G. 1990. Active thrusting and folding in the Qilian Shan,and decoupling between upper crust and mantle in northeastern Tibet[J]. Earth Planet Sci Lett,97(3/4):382–403.
    Tapponnier P,Xu Z Q,Roger F,Meyer B,Arnaud N,Wittlinger G. 2001. Oblique stepwise rise and growth of the Tibet Plateau[J]. Science,294(5547):1671–1677. doi: 10.1126/science.105978
    Wei S J,Helmberger D,Avouac J P. 2013. Modeling the 2012 Wharton basin earthquakes off-Sumatra:Complete lithospheric failure[J]. J Geophys Res:Solid Earth,118(7):3592–3609. doi: 10.1002/jgrb.50267
    Wessel P,Luis J F,Uieda L,Scharroo R,Wobbe F,Smith W H F,Tian D. 2019. The Generic Mapping Tools version 6[J]. Geochem Geophys Geosyst,20:5556–5564.
    Wang M,Shen Z K. 2020. Present-day crustal deformation of continental China derived from GPS and its tectonic implications[J]. J Geophys Res:Solid Earth,125(2):e2019JB018774.
    Xu X W,Yeats R S,Yu G H. 2010. Five short historical earthquake surface ruptures near the Silk Road,Gansu Province,China[J]. Bull Seismol Soc Am,100(2):541–561. doi: 10.1785/0120080282
    Zhang P Z,Molnar P,Xu X W. 2007. Late Quaternary and present-day rates of slip along the Altyn Tagh fault,northern margin of the Tibetan Plateau[J]. Tectonics,26(5):TC5010.
    Zhang W Q,Jiao D C,Zhang P Z,Molnar P,Burchfield B C,Deng Q D,Wang Y P,Song F M. 1987. Displacement along the Haiyuan fault associated with the great 1920 Haiyuan,China,earthquake[J]. Bull Seismol Soc Am,77(1):117–131.
    Zheng W J,Zhang P Z,He W G,Yuan D Y,Shao Y X,Zheng D W,Ge W P,Min W. 2013. Transformation of displacement between strike-slip and crustal shortening in the northern margin of the Tibetan Plateau:Evidence from decadal GPS measurements and Late Quaternary slip rates on faults[J]. Tectonophysics,584:267–280. doi: 10.1016/j.tecto.2012.01.006
    Zheng X J, Zhang Y, Wang R J, Zhao L, Li W Y, Huang Q H. 2020. Automatic inversions of strong-motion records for finite-fault models of significant earthquakes in and around Japan[J]. J Geophys Res: Solid Earth, 125（9）: e2020JB019992.
    Zhu L P,Rivera L A. 2002. A note on the dynamic and static displacements from a point source in multilayered media[J]. Geophys J Int,148(3):619–627. doi: 10.1046/j.1365-246X.2002.01610.x
    • Related Articles

  • Related Articles

    Yao Yuan, Yang Zhousheng, Zhou Shiyong. 2023: Seismicity in Zemuhe fault zone based on dense seismic array. Acta Seismologica Sinica, 45(6): 985-995. DOI: 10.11939/jass.20220084
    Zhu Lin, Dai Yong, Shi Fuqiang, Shao Huicheng. 2022: Coulomb stress evolution and seismic hazards along the Qilian-Haiyuan fault zone. Acta Seismologica Sinica, 44(2): 223-236. DOI: 10.11939/jass.20220012
    He Yicheng, Peng Xiaobo, Xia Wenjun, Huo zhuqing, Chen Nan, Xu Nian. 2020: Inversion method and application of seismic intensity attenuation parameters based on genetic algorithm. Acta Seismologica Sinica, 42(4): 435-446. DOI: 10.11939/jass.20190171
    Wang Jinyan, Lu Renqi, Zhang Hao, Li Juhong, Li Limei, Xu Hangang, Gu Qinping, Shu Peng, Hou Ying. 2020: Three-dimensional geological modeling of Cenozoic erathem in Jiangsu segment of the Tanlu fault zone. Acta Seismologica Sinica, 42(2): 216-230. DOI: 10.11939/jass.20190131
    Xia Tingting, Zhang Jingfa, Tian Tian. 2019: Three-dimensional modeling of the crust structure of Longmenshan fault zone. Acta Seismologica Sinica, 41(6): 743-756. DOI: 10.11939/jass.20190087
    Li Jiaxin, Hong Qiyu, Zheng Xuyao. 2017: Study on the deep seismic wide-angle reflection/refraction profile in the middle of Longmenshan fault zone. Acta Seismologica Sinica, 39(2): 188-206. DOI: 10.11939/jass.2017.02.003
    Hu Gang, He Zhengqin, Li Na, Ye Tailan. 2016: Detection of the northern section of Anninghe fault zone by seismic reflection method. Acta Seismologica Sinica, 38(6): 813-823. DOI: 10.11939/jass.2016.06.001
    Shao Yanxiu, Yuan Daoyang, Liang Mingjian. 2015: Seismic risk assessment of Longling-Lancang fault zone， southwestern Yunnan. Acta Seismologica Sinica, 37(6): 1011-1023. DOI: 10.11939/jass.2015.06.011
    Lian Weiping, Li Li, Tang Fangtou, Hu Bin, Li Xiaoxuan. 2014: A finite element analysis method for the numerical simulation of characteristic earthquakes: Case study based on the Longmenshan fault zone. Acta Seismologica Sinica, 36(6): 1010-1021. DOI: 10.3969/j.issn.0253-3782.2014.06.003
    He Zhengqin, An Haoshou, Shen Kun, Lu Laiyu, Hu Gang, Ye Tailan. 2013: Detection of Puduhe fault in Yuxi basin of Yunnan by seismic reflection method. Acta Seismologica Sinica, 35(6): 836-847. DOI: 10.3969/j.issn.0253-3782.2013.06.007

Catalog

    Get Citation
    PDF
    XML
    Article views (668) PDF downloads (182) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles

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

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return