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《SEISMOLOGICAL RESEARCH OF NORTHEAST CHINA》 1998-03
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DETERMINANIING STRESS AXIS OF FAULT ACTIVITY AND STRESS FIELD OF CAPITAL CIRCLE

Guo Liangqian (First Land Deformation Monitoring Center SSB Tianjin 300180)  
The formula calculating the direction of horizontal main stress about fault activity has been given by fault deformation data on the basis of stress-strain relation. Having used the deformation data of seismic faults for Xingtai, Haicheng and earthquake, their main stress direction has been obtained, respectively, The results are consistent with their earthquake focal mechanism. The horizontal main stress axises of capital circle area are also calculated by the data of crossing fault. The results show that superior direction of main stress is 50°~70°, and there exists no obvious change for ten years.
【Fund】: 国家地震局95-04-07-03-04项目资助
【CateGory Index】: P315.1
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【References】
Chinese Journal Full-text Database 3 Hits
1 LIU Guan-zhong1,WANG Jian-jun1,WANG Zai-hua2,JIANG jing-xiang2,XIE Zhou-min1,CHEN Zhao-liang3(1.Institute of Crustal Dynamics,China Seismological Bureau,Beijing 100085,China)(2.Seismological Bureau of Xinjiang Uygur Autonomous Region,Urumqi 830011,Xinjiang,China)(3.Kuitun Seismostation,Earthquake Administration of Xinjiang Yili Prefecture,Kuitun 833200,Xinjiang,China);Movement Character and Deformation Anomaly Research of Dushanzi-Anjihai Fault Nowadays[J];地震研究;2009-02
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【Co-citations】
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1 LIU Zhongya;PENG Xuanming;ZHAO Tiehu;SUN Jun;Chinese Academy of Geological Sciences;Qingdao Institute of marine Geology;;THE DISTRIBUTION AND ACTIVITIES OF ACTIVE FAULTS IN THE BOHAI STRAIT AND ITS ADJACENT AREAS[J];海洋地质与第四纪地质;2016-01
2 Liu Yanxia;Qi Yali;Huang Haijun;Bi Haibo;Yan Liwen;Ma Lijie;Key Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of Sciences;Guangdong Ocean University;;RECONSTRUCTION AND DIFFERENTIATION FACTOR OF PALEOSHORELINE FOR THE SOUTHWESTERN OF THE BOHAI SEA IN 6ka B.P.[J];第四纪研究;2015-02
3 LIU Gui-wei1,2,3,HUANG Hai-jun1,2,DU Ting-qin4,BIE Jun2,CHEN Ji-tao5(1.Key Laboratory of Marine Geology and Environment,the Chinese Academy of Sciences,Qingdao 266071,China;2.Institute of Oceanology,the Chinese Academy of Sciences,Qingdao 266071,China;3.Gradute School of the Chinese Acadamy of Sciences,Beijing 100039,China;4.Shandong Academy of Environmental Science,Jinan 250013,China;5.Hydrology and Water Resources Bureau of Shandong,Jinan 250010,China);Effective factors of land subsidence in the Yellow River Delta[J];海洋科学;2011-08
4 Guo Liangqian (First Land Deformation Monitoring Center SSB Tianjin 300180);DETERMINANIING STRESS AXIS OF FAULT ACTIVITY AND STRESS FIELD OF CAPITAL CIRCLE[J];东北地震研究;1998-03
5 Wang Weiping(Aerogeophysical Survey and Remote--Sensing Center, Ministry of Geology and Mineral Resources, Beijing 100083);A PRELIMINARY STUDY ON CRUSTAL STRUCTURE AND CRUSTAL STABILITY OF WESTERN LIAONING ARSA[J];物探与化探;1997-05
6 Zhang Cun-de and Xiang Jia-cui (Institute of Geology, State Seismological Bureau, Beijing, 100029);ON THE RECENT TECTONIC MOVEMENT IN NORTH CHINA[J];地震地质;1990-03
7 Wang Li(Station of Remote Sensing Geology, Bureau of Geology and Mineral Resources of Liaoning);A DISCUSSION ON THE STABILITY OF THE REGIONAL CRUST WITH INTERPRETATION ON STRUCTURES BY REMOTE SENSING IMAGES IN YINGKOU AREA[J];辽宁地质;1988-04
8 Jiang Zhaohuai Wu Qinglin (Seismoloflical Bureau of Jiangsu Province);A STUDY ON THE RELATIONSHIP BETWEEN CHANGES OF THE SEA LEVEL IN THE COAST OF EAST CHINA AND EARTHQUAKES[J];地壳形变与地震;1988-02
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1 LIU Guan-zhong1,JIANG Jing-xiang2,WANG Jian-jun1,WANG Zai-hua2 (1.Institute of Crustal Dynamics,CEA,Beijing 100085,China;2.Earthquake Administration of Xinjiang Uygur Autonomous Region,Urumqi 830011,Xinjiang,China);"RATE CUMULATION ANALYSIS" ON CROSS-FAULT FIXED DEFORMATION DATA AND ANOMALY EXTRACTION METHOD[J];内陆地震;2007-03
2 JIAO Qing1,ZHANG Hong-xu1,SONG Guang-fu2,JING Yan1,FAN Guo-sheng1 (1.Institute of Crustal Dynamics,CEA,Beijing 100085;2.Earthquake Administration of Xinjiang Uigur Autonomous Region,Urumqi 833200,China);A preliminary study on the cross-fault displacement variation at Dushanzi Station in Xinjiang,China,before the M7.8 earthquake in Pakistan[J];地震;2007-01
3 LI Zu-ning WU Shao-zu CHEN Guang ZHONG Ji-mao YUAN Li-wen(Earthquake Administration of Fujian Province, Fuzhou 350003, China);Study of Across-fault Short Leveling Anomalous Data in Tianma, Xiamen, Fujian, by Using Integral Point Load Method[J];地震研究;2007-01
4 Cui Xiaofeng (Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China);CHARACTERISTICS OF RECENT TECTONIC STRESS FIELD IN JIASHI, XINJIANG AND ADJACENT REGIONS[J];地震学报;2006-04
5 JING Yan~(1,2) REN Jin-wei~3 WANG Hui~3(1.School of the Earth Sciences and Resourses,China University of Geoscience,Beijing 100083,China)(2.Institute of Crustal Dynamics,CEA,Beijing 100085,China)(3.Institute of Earthquake Prediction,CEA,Beijing 100036,China);Tectonic Deformation of China Continent and Its Adjacent Regions since Late Pleistocene Inferred from Active Fault Movement Data[J];地震研究;2005-04
6 YANG Yong-lin,SU Qin,ZHU Hang(Engineering Institute of Surveying and Mapping,Earthquake Administration of Sichuan Province,SichuanYaan 625000, China);Active characteristic of several faults in Yunnan and Sichuan Provinces based on the results from the observation data of both leveling and base line[J];四川地震;2005-03
7 CUI Xiao-feng XIE Fu-ren ZHAO Jian-tao (Institute of Crustal Dynamics, CEA, Beijing 100085, China);THE REGIONAL CHARACTERISTICS OF FOCAL MECHANISM SOLUTIONS IN CHINA AND ITS ADJACENT AREAS[J];地震地质;2005-02
8 WANG Zai-hua1, KONG De-feng2, SONG Guang-fu2(1. Seismological Bureau of Xinjiang Uygur Autonomous Region, Urumqi 830011, Xinjiang, China; 2. Kuitunstation of Seismological Bureau of Yili Kazak Autonomous Canton, Kuitun 833200, Xinjiang, China);RALATIVE ANALYSIS BETWEEN FAULT DEFORMATION OBSERVATIONAL DATUM AND AUXILIARY TEMPERATURE OBSERVATIONAL DAUTM[J];内陆地震;2005-02
9 JIANG Jing-xiang~1,WANG Zai-hua~1,WEN He-ping~1,YANG You-ling~1, WANG Rui-ping~2,WANG Ai-qian~3,LAI Ai-jing~4 (1.Earthquake Administration of Xinjiang Uygur Autonomous Region, Urumqi 830011; 2.Seismic Station of Akesu, Akesu 843000; Management Bureau of Kizil Reservoir of Xinjiang, Baicheng 8423123; 4. Seismic Station of Wushi, Wushi 843400, China);Preliminary analysis of anomalies of fixed point deformation before Zhaosu M_S6.0 earth- quake on December 1, 2003[J];地震;2005-02
10 JING Yan 1,2 ZHAO Ying-hai 1 ZHANG Hong-xu 1 SONG Guang-fu 3 WANG Zai-hua 4 WANG Feng 5 (1. Institute of Crustal Dynamics, CEA, Beijing 100085, China) ( 2. School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China) (3. Kuitun Seismostation, Earthquake Administration of Xinjiang Yili Prefecture, Kuitun 833200, China) (4. Earthquake Administration of Xinjiang Uygur Automomous Region, Urumqi 830011, China) (5.China Earthquake Administration, Beijing 10036,China);Monitoring of Dushanzi-Anjihai Fault with Single-baseline, Two-component, Obliquely-crossing-fault Instruments[J];地震研究;2005-02
【Secondary References】
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1 Liu Sha;Wu Peng;Institute of Geophysics,China Earthquake Administration;Sichuan Earthquake Agency;;Changes of shear-wave splitting parameters in Jinping hydro-power station, Sichuan[J];地震学报;2018-01
2 GUO Xiangyun;JIANG Changsheng;WANG Xiaoshan;TIAN Xin;Institute of Geophysics,CEA;Earthquake Administration of Hebei Province;;Characteristics of Small to Moderate Focal Mechanism Solutions Stress Field of the Circum-Ordos Block[J];大地测量与地球动力学;2017-07
3 ZHENG Tuo;DING Zhi-Feng;CHANG Li-Jun;ZHENG Chen;ZHANG Hui;LI Da-Hu;Institute of Geophysics,China Earthquake Administration;School of Earth and Space Sciences,Peking University;Key Laboratory of Seismic Observation and Geophysical Imaging,China Earthquake Administration;Shandong Province Changyi Seismic Station;Earthquake Administration of Sichuan Province;;S-wave splitting in upper crust near the scientific drilling WFSD-3 at the Wenchuan earthquake fault zone[J];地球物理学报;2017-05
4 MIAO Qingjie;GAO Yuan;LIU Xiqiang;QU Junhao;ZHENG Jianchang;Earthquake Administration of Shandong Province;Institute of Earthquake Science,CEA;;Tectonic Stress Analysis Based on the Crustal Seismic Anisotropy in Rushan Earthquake Near-Field Region[J];大地测量与地球动力学;2017-03
5 LI Jin;GAO Yuan;ZHANG Bo;WANG Liang;GAO Rong;Earthquake Administration of Xinjiang Uygur Autonomous Region;Institute of Earthquake Science,China Earthquake Adiministration;Earthquake Administration of Liaoning Province;;THE SHEAR-WAVE SPLITTING OF GAIZHOU EARTHQUAKE SWARM IN LIAONING[J];地震地质;2016-04
6 Yang Zhigao;China Earthquake Networks Center;;Study on the August 14,2015 Changli M_S4.2 earthquake and crust stress of its nearby region[J];中国地震;2016-04
7 Miao Qingjie;Liu Xiqiang;Earthquake Administration of Shandong Province;;Temporal variation characteristics of shear-wave splitting for the Rushan earthquake swarm of Shandong Province[J];地震学报;2016-02
8 WANG Xia;SONG Mei-qin;WANG Liang;LI Hong-wei;WU Hao-yu;LUO Yong;Earthquake Administration of Shanxi Province;State Key Laboratory of Geodesy and Earth's Dynamics,Institute of Geodesy and Geophysics,Chinese Academy of Sciences;Earthquake Administration of Liaoning Province;;STUDY ON CRUSTAL VELOCITY STRUCTURE BENEATH KOUQUAN FAULT AND ADJACENT AREA[J];地震地质;2015-04
9 LIU Sha;WU Peng;Institute of Geophysics,China Earthquake Administration;Earthquake Administration of Sichuan Province;;The effect of water level changes in Zipingpu reservoir on the parameters of shear wave splitting[J];地球物理学报;2015-11
10 GUO Gui-Hong;ZHANG Zhi;CHENG Jian-Wu;DONG Zhi-Ping;YAN Jian-Ping;MA Ya-Wei;The Key Laboratory of Mechanics on Disaster and Environmental in Western China & Lanzhou University;Lanzhou National Observatory of Geophysics;Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration,College of Earth Sciences & Guilin University of Technology;Lanzhou Institute of Seismology,China Earthquake Administration;School of Earth Sciences & Lanzhou University;;Seismic anisotropy in the crust in northeast margin of Tibetan Plateau and tectonic implication[J];地球物理学报;2015-11
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