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Formation Mechanism of Ground Fissures Originated from the Hanging Wall of Normal Fault:A Case in Fen-Wei Basin,China

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Journal of Earth Science 2022年第2期33卷 482-492页

作者： Zhijie Jia Jianbing Peng Quanzhong Lu Jianwei Qiao Feiyong Wang Mingdong Zang Yang Liu Junyan Zhao Fengji Zhu School of Geological Engineering and Geomatics Chang an UniversityXi'an 710054China Key Laboratory of Western Mineral Resources and Geological Engineering Ministry of Education Chang'an UniversityXfan 710064China China JK Institute of Engineering and Design Xfan 710043China Shaanxi Key Laboratory for the Property and Treatment of Special Soil and Rock Xfan 710043China School of Engineering and Technology China University of GeosciencesBeijing 100083China

This paper takes Fen-Wei Basin(FWB)as a case to study the ground fissures controlled by normal *** on the field investigation,geophysical exploration,drilling,GNSS data and numerical calculation,the characteristics and mechanism of ground fissures originated from the hanging wall of normal faults are *** results show that the distribution of ground fissures in the hanging wall and heading wall of the active faults is not *** fissures are mostly distributed in the hanging wall of active faults and show a linear distribution on the surface,their strike is consistent with the fault,mainly characterized by vertical offset and horizontal *** fissures destroy the farmland and building foundation through which they pass and cause the rupture or *** profile section,the ground fissure shows the characteristics of normal faults and dislocates the strata,and is connected with the underlying *** analysis shows that the vertical displacement of normal fault activity in hanging wall is much larger than that in heading wall,which is the reason that tectonic ground fissures mainly originate from hanging *** range of dangerous area of ground fissures is controlled by the depth of fault,the strength of the ground fissures disaster is mainly controlled by the activity of *** formation of the ground fissures originated from the hanging wall of the fault experienced three stages:the main fault activity stage,the secondary fault activity stage and the fissure formation stage.

关键词： ground fissure Fen-Wei Basin active fault dislocation theory formation mechanism hazards engineering geology

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Effects of Earth's curvature and radial heterogeneity in dislocation studies:Case studies of the 2008 Wenchuan earthquake and the 2004 Sumatra earthquake

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Earthquake Science 2010年第4期23卷 301-308页

作者： Guangyu Fu Wenke Sun Yoichi Fukuda Shanghua Gao Takashi Hasegawa Institute of Earthquake Science China Earthquake Administration Beijing 100036 China Department of Geophysics Graduate School of Science Kyoto University Kyoto 606-8502 Japan Laboratory of Computational Geoclynamics Graduate University of Chinese Academy of Sciences Beijing 100049 China

Recently, effects of Earth＇s curvature and radial heterogeneity on coseismic deformations are often investi- gated based on the 2004 Sumatra earthquake. However, such effects are strongly related to earthquake types. As a low dip angle event, the 2004 Sumatra earthquake is not a good seismic case for such a topic since the effects for moderate dip angle events are much bigger. In this study, the half-space and spherical dislocation theories are used, respectively, to calculate co- seismic displacements caused by the 2008 Wenchuan earthquake and the 2004 Sumatra earthquake. Effects of Earth＇s curva- ture and stratification are investigated through the discrepancies of results calculated using the two dislocation theories. Re- sults show that the effects of Earth＇s curvature and stratification for the 2008 Wenchuan earthquake are much larger than those for the 2004 Sumatra earthquake. Ignoring the effects will cause errors up to 100%-200% in far field displacements for a moderate dip angle event like the 2008 Wenchuan earthquake. Such great effects are much bigger than those conclusions of previous studies. Besides, comparison with observations verifies that spherical dislocation theories yield better results than half-space ones in far fields.

关键词： coseismic displacement dislocation theory Earth model

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Co-seismic strain changes of Wenchuan Mw7.9 earthquake recorded by borehole strainmeters on Tibetan plateau

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Geodesy and Geodynamics 2011年第3期2卷 42-49页

作者： Fu Guangyu Shen Xuzhang Fukuda Yoichi Gao Shanghua Yoshii Satoshi Institute of Earthquake Sciences China Earthquake Administration Beijing 100036 China Key Laboratory of Computational Geodynamics Chinese Academy of Sciences Belting 100049 China Lanzhou Institute of Seismology China Earthquake Administration Lanzhou 730000 China Department of Geophysics Graduate School of Science Kyoto University Kyoto 6068502 Japan

Co-seismic strain changes of the Wenchuan MwT. 9 earthquake recorded with three four-component borehole strainmeters showed NW-SE and roughly EW extensions, respectively, at two locations in the interior and northern part of Tibetan plateau, and NS shortening at a location south of the epicenter, in agreement with the tectonic stress field of this region retical values obtained with half-space effects, such as local crustal structure The observed values of as much as 10-7 are, however, larger than theo- and spherical-earth dislocation theories, implying the existence of other and initial stress.

关键词： Wenchuan MwT. 9 earthquake co-seismic strain changes Tibetan plateau dislocation theory

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Simulation of co-seismic gravity change and deformation of Wenchuan Ms8.0 earthquake

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Geodesy and Geodynamics 2010年第1期1卷 8-14页

作者： Chongyang Shen Hui Li Hongbo Tan Institute of Seismology China Earthquake Administration Wuhan 430071 China Crustal Movement Laboratory Wuhan 430071 China

Surface co-seismic gravity changes and displacements caused by the Wenchuan Ms8.0 earthquake are calculated on the basis of the half-space dislocation theory and two fault models inversed, respectively, by Institute of Geophysics, CEA and USGS. The results show that 1 ） the dislocation consists of dip slip and rightlateral strike slip ;2 ）the co-seismic gravity change shows a four-quadrant pattern ,which is greatly controlled by the distribution of the vertical displacements, especially in the near-filed ; 3 ） the gravity change is generally less than 10 × 10^-8 ms^-2 in the far-field,but as high as several 100 × 10^-8 ms^-2 in the near-filed. These results basically agree with observational results.

关键词： Wenchuan earthquake dislocation theory gravity change deformation simulation

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Simulation of coseismic effects of the Ms7. 0 Lushan earthquake

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Geodesy and Geodynamics 2013年第3期4卷 12-18页

作者： Tan Hongbo Shen Chongyang Wei Jin Zhao Bin Wang Jian Xuan Songbai Key Laboratory of Earthquake Geodesy Institute of SeismologyChina Earthuake Administration Wuhan Bace of Institute of Crustal Dynamics China Earthquake Administration

Using plane dislocation theory and the seismic-wave inversion results from the Institute of Geophysics, China Earthquake Administration and the Institute of Geodesy and Geophysics, Chinese Academy of Sciences models, the surface coseismic deformation and gravity changes caused by the 2013 Ms7.0 Lushan earthquake are simulated. The simulations of coseismic gravity change and deformation indicate that the dislocation has dip-slip characteristics. The results also show that the coseismic deformation exhibits a symmetrical, positive-and-negative distribution, with the deformation usually being less than 10 mm in the far- field but up to 140 mm in the near-field. The gravity changes are concentrated on the fault-projection area, which is greatly affected by the vertical surface deformation. The gravity change and vertical deformation in the far field are usually less than and 5 mm, respectively, but reach and 330 mm, respectively, in the near field. The simulated results agree well with the measured resuhs, which suggests a theoretical basis for the observed change in gravity before and after this earthquake.

关键词： Lushan earthquake dislocation theory coseismic effects simulation

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Far-field deformations caused by the 2004 Sumatra earthquake

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Geodesy and Geodynamics 2010年第1期1卷 70-78页

作者： Guangyu Fu Wenke Sun Institute of Earthquake Science China Earthquake Administration Beijing 100036 China Laboratory of Computational Geodynamics Graduate University of Chinese Academy of Sciences Beijing 100049 China

Theoretical horizontal displacements caused by the 2004 Sumatra earthquake in the Sichuan-Yunnan area have been calculated according to a spherical dislocation theory and an earthquake-fault model. The results show that the theoretical displacements are basically consistent with the GPS observations in situ. On this basis,we have calculated the co-seismic displacements, strains, changes of gravity and geoid of the whole Earth, including China mainland and vicinity, caused by this earthquake. Key wards：

关键词： the 2004 Sumatra earthquake dislocation theory displacement strain gravity change far-field deformation

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A Mesh-Independent Brute-Force Approach for Traction-Free Corrections in dislocation Problems

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Modeling and Numerical Simulation of Material Science 2021年第1期11卷 1-18页

作者： Abu Bakar Siddique Tariq Khraishi Mechanical Engineering Department University of New Mexico New Mexico USA

Simulation of dislocation dynamics opens the opportunity for researchers and scientists to observe in-depth many plastic deformation phenomena. In 2D or 3D media, modeling of physical boundary conditions accurately is one of the keys to the success of dislocation dynamics (DD) simulations. The scope of analytical solutions is restricted and applies to specific configurations only. But in dynamics simulations, the dislocations’ shape and orientation change over time thus limiting the use of analytical solutions. The authors of this article present a mesh-based generalized numerical approach based on the collocation point method. The method is applicable to any number of dislocations of any shape/orientation and to different computational domain shapes. Several verifications of the method are provided and successful implementation of the method in 3D DD simulations have been incorporated. Also, the effect of free surfaces on the Peach-Koehler force has been computed. Lastly, the effect of free surfaces on the flow stress of the material has been studied. The results clearly showed a higher force with increased closeness to the free surface and with increased dislocation segment length. The simulations’ results also show a softening effect on the flow stress results due to the effect of the free surfaces.

关键词： Free Surfaces dislocation theory dislocation Dynamics Peach-Koehler Force

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