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The surface rupture zone and Coseismic Deformation Produced by the Yutian Ms7.3 Earthquake of 21 March 2008,Xinjiang

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Acta Geologica Sinica(English Edition) 2012年第1期86卷 256-265页

作者： SHAN Xinjian QU Chunyan WANG Chisheng ZHANG Guifang ZHANG Guohong SONG Xiaogang GUO Liming LIU Yunhua State Key Laboratory of Earthquake Dynamics Institute of GeologyChina Earthquake Administration Beijing 100029China Institute of Remote Sensing Application Chinese Academy of SciencesBeijing 100101China

On 21 March 2008, a Ms7.3 earthquake occurred at Quickbird, Yutian County, Xinjiang. We attempt to reveal the features of the causative fault of this shock and its coseismic deformation field. Our work is based on analysis and interpretation to high-resolution satellite images as well as differential interferometric synthetic aperture radar （D-InSAR） data from the satellite Envisat SAR, coupled with seismicity, focal mechanism solutions and active tectonics in this region. The result shows that the 40 km-long, nearly NS trending surface rupture zone by this event lies on a range-front alluvial platform in Qira County. It is characterized by distinct linear traces and simple structure with 1-3-m-wide individual seams and maximum 6.5 m width of a collapse fracture. Along the rupture zone many secondary fractures and fault-bounded blocks are seen, exhibiting remarkable extension. The eoseismic deformation affected a large area 100~100 km2. D-InSAR analysis indicates that the interferometric deformation field is dominated by extensional faulting with a small strike-slip component. Along the causative fault, the western wall fell down and the eastern wall, that is the active unit, rose up, both with westerly vergence. Because of the big deformation gradients near the seismogenic fault, no interference fringes are seen on images, and what can be determined is a vertical displacement 70 cm or more between the two fault walls. According to the epicenter and differential occurrence times from the National Earthquake Information Center, China Earthquake Network Center, Harvard and USGS, it is suggested that the seismic fault ruptured from north to south.

关键词： Yuntian Earthquake high resolution image D-InSAR surface rupture zone coseismic deformation field

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The Emergency Scientific Investigation on the surface rupture zone of the M_S 7.1 Yushu Earthquake

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Earthquake Research in China 2011年第4期25卷 521-524页

作者： Wang Ji Chen Lichun Tian Qinjian Li Zhimin Sun Xinzhe Zhang Xiaoqing China Earthquake Disaster Prevention Center Beijing 100029 China Institute of Geology China Earthquake Administration Beijing 100029 China Earthquake Administration of Qinghai Province Xining 810001 China

The coseismic surface rupture zone of the seismogenic fault of the Ms7.1 Yushu earthquake includes three left-stepping main ruptures, striking 300°- 320°, in general. An approximately 2km-long en echelon tension fissure zone was found at Longbao town. The main rupture in the northern part is about 16km long, about 9kin long in the middle part, and about 7km long in the southern part, with a total length of 34km. Each of the main ruptures consists of a series of en echelon sub-ruptures represented by a series of compression bulges alternating with tension fissures or by en echelon fissures. The rupture at Changusi, the southernmost of the ruptures, is characterized by vertical displacement, with a value of 50cm. The rupture zone shows left-lateral strike-slip characteristics. The maximal horizontal slip is on the northern main rupture, with a value of 1.8m.

关键词： Ms7. 1 Yushu earthquake surface rupture zone Emergency scientificinvestigation

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Holocene activities of the Taigu fault zone,Shanxi Province, and their relations with the 1303 Hongdong M=8 earthquake

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Acta Seismologica Sinica(English Edition) 2004年第3期17卷 308-321页

作者： XIE Xin-sheng(谢新生) JIANG Wa-li(江娃利) WANG Huan-zhen(王焕贞) FENG Xi-ying(冯西英) Institue of Crust Dynamics China Earthquake AdministrationBeijing100085China Institue of Crust DynamicsChina Earthquake AdministrationBeijing100085China Institue of Crust DynamicsChina Earthquake AdministrationBeijing100085China Institue of Crust DynamicsChina Earthquake AdministrationBeijing100085China

No abstract available

关键词： Taigu fault Holocene activities 1303 Hongdong earthquake surface rupture zone

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Late-Quaternary strong earthquakes on the seismogenic fault of the 1976 M_s7.8 Tangshan earthquake,Hebei,as revealed by drilling and trenching

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Science China Earth Sciences 2011年第11期54卷 1696-1715页

作者： GUO Hui JIANG WaLi XIE XinSheng Institute of Crustal Dynamics China Earthquake Administration Beijing 100085 China

Composite borehole profiling combined with trenching is an effective way to acquire evidence of past ruptures of buffed active faults. In this study, three composite borehole profiles and a large-scale trench excavation were carded out across the surface rupture zone of the 1976 Ms7.8 Tangshan earthquake. The following three major conclusions have been reached. （1） The surface rupture zone of the 1976 earthquake extends more than 47 km long to the south of Tangshan city, passing to the west of Sunjialou, to Daodi town in Fengnan County, to Xihe in Fengnan County. （2） The surface rupture zone is divided into south and north branches. The north branch has mainly fight-lateral strike-slip motion, and the vertical displacement of the surface is up on the west and down on the east. On the other hand, the vertical displacement of the south branch is up on the east and down on the west, accompanied by some right-lateral slip. Such a faulting style cannot be explained by the movement of a single normal or reverse fault, but is consistent with the vertical displacement field induced by the fight-lateral strike-slip of the fault belt. The drilling and trenching data from this study verify that such activity continued through the Late Quaternary on the Tangshan Fault. （3） The fault planes exhumed by trenching and the dislocations of strata revealed by the boreholes indicate that multiple faulting events occurred on the Tangshan Fault in the Late Quaternary. The timing of three ruptures prior to the 1976 earthquake was 7.61-8.13, 〉14.57, and 24.21-26.57 ka BP. Counting the earthquake of 1976, the recurrence interval of the four strong events is about 6.7 to 10.8 ka. On one of the three borehole profiles, the Niumaku profile, nine faulting events were detected since 75.18 ka BP with an average interval of 8.4 ka. In addition, this paper also discusses the difference between the Late Quaternary sedimentary environments to the north and south of Tangshan city based on stratum dati

关键词： Tangshan earthquake surface rupture zone multi-stage activity earthquake recurrence interval paleoseismic trench-ing borehole profile

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Parameters of Coseismic Reverse- and Oblique-Slip surface ruptures of the 2008 Wenchuan Earthquake,Eastern Tibetan Plateau

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Acta Geologica Sinica(English Edition) 2009年第4期83卷 673-684页

作者： XU Xiwei YU Guihua CHEN Guihua RAN Yongkang LI Chenxia CHEN Yuegau CHANG Chungpai Institute of Geology China Eathquake Administrative Beijing 100029 Department of Geosciences National Taiwan University Taipei Center for Space and Remote Sensing Research National Central University Jhongli Taipei

On May 12th, 2008, the Mw7.9 Wenchuan earthquake ruptured the Beichuan, Pengguan and Xiaoyudong faults simultaneously along the middle segment of the Longmenshan thrust belt at the eastern margin of the Tibetan plateau. Field investigations constrain the surface rupture pattern, length and offsets related to the Wenchuan earthquake. The Beichuan fault has a NE-trending rightlateral reverse rupture with a total length of 240 km. Reassessment yields a maximum vertical offset of 6.5±0.5 m and a maximum right-lateral offset of 4.9±0.5 m for its northern segment, which are the largest offsets found; the maximum vertical offset is 6.2±0.5 m for its southern segment. The Pengguan fault has a NE-trending pure reverse rupture about 72 km long with a maximum vertical offset of about 3.5 m. The Xiaoyudong fault has a NW-striking left-lateral reverse rupture about 7 km long between the Beichuan and Pengguan faults, with a maximum vertical offset of 3.4 m and left-lateral offset of 3.5 m. This pattern of multiple co-seismic surface ruptures is among the most complicated of recent great earthquakes and presents a much larger danger than if they ruptured individually. The rupture length is the longest for reverse faulting events ever reported.

关键词： surface rupture zone coseismic offset Wenchuan earthquake Longmenshan

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Exploration of Suspected surface ruptures of the M_S8.0 Wenchuan Earthquake at Frontal Areas of Longmenshan Using Shallow Seismic Reflection

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Earthquake Research in China 2009年第3期23卷 299-309页

作者： Liu Baojin Yang Xiaoping Feng Shaoying Kou Kunpeng Geophysical Prospecting Center China Earthquake Administration Zhengzhou 450002 China Institute of Geology China Earthquake AdministrationBeijing 100029China

The great M_S8.0 Wenchuan earthquake on May 12,2008 was generated by abrupt faulting in the Yingxiu-Beichuan fault along the Longmenshan fault zone. The earthquake not only produced surface ruptures along the Yingxiu-Beichuan and Guanxian-Jiangyou faults,but also surface ruptures,arching of highway pavement,sand-boils and waterspouts in various degrees in areas such as Shifang and Mianzhu on the Chengdu Plain. To understand the shallow geological structures under the surface rupture zone,a 6350m long high-resolution shallow seismic reflection profile in near-EW direction was performed. This profile is located at Shigu town,Shifang city,where a suspected earthquake surface rupture zone was discovered. In this study,a group interval of 3m,shotpoint interval of 18m,and a 300-channel 25-fold observation system were used. In consideration of both near-surface reflections and dipping interface imaging,we adopted the split-spread geometry and asymmetrical zero-offset receiving technique. To better suppress random-noise and raise the signal-to-noise ratio of seismic data,30 times vertical stacking of vibrator signals was made for each common-shot gather after correlation of individual records. By using the above work method and spread geometry,we obtained high-resolution images of structures in the depth range of 15m～800m after data processing. The result shows the existence of buried thrust faults thrusting to the plain area and back-thrust faults under the surface rupture zone. It also shows that the activity of the buried thrust faults may be the main cause for folding and deformation in near-surface strata and coseismic surface rupturing.

关键词： Ms8.0 Wenchuan earthquake surface rupture zone Shallow seismic reflectionprofile Buried thrust fault

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