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《Geotechnical Investigation & Surveying》 2016-10
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Study of crustal deformation in southeastern Gansu

Zhou Lin;Hao Ming;Qin Shanlan;Song Shangwu;Second Crust Monitoring and Application Center,CEA;Institute of Disaster Prevention;  
The study of crustal deformation in southeastern Gansu is based on the GPS data observed since2009 to 2014. The crustal movement results show that the horizontal velocity direction is mainly in NEEEW-SE and the crust is in a compression state. The strain field shows that Pingwu-Qingchuan fault has the highest values which is up to 3. 5 × 10- 8/ a,Lintan-Tanchang fault and Lixian-Luojiabao fault also have relative high values. At Liupanshan fault,the crustal shortening is more obvious.
【Fund】: 中国地震局监测预报专项(16A38ZX281)
【CateGory Index】: P227;P228.4
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【Citations】
Chinese Journal Full-text Database 5 Hits
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【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 Zhou Lin;Hao Ming;Qin Shanlan;Song Shangwu;Second Crust Monitoring and Application Center,CEA;Institute of Disaster Prevention;;Study of crustal deformation in southeastern Gansu[J];工程勘察;2016-10
2 XU Wan-zhen;MENG Guo-jie;SU Xiao-ning;Institute of Earthquake Science,CEA;College of Surveying and Geo-informatics,Tongji University;;Interseismic Locking Characteristics of the Liupanshan Fault from GPS Observation[J];地震;2016-03
3 LI Qing-mei;ZHANG Yuan-sheng;LV Jun-qiang;XIE Hui;LI Hong-ting;ZHAO Wei-dong;Earthquake Administration of Ningxia Hui Autonomous Region;Lanzhou Institute of Seismology,CEA;;Relocation of Small Earthquakes in the Ningxia Area[J];地震工程学报;2015-02
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7 WAN Yong-Ge~(1,2),SHENG Shu-Zhong~(1,2),HSU Ya-Ju~3,WU Yih-Min~4 1 Institute of Disaster Prevention,Hebei Sanhe 065201,China 2 Institute of Geophysics,China Earthquake Administration,Beijing 10081,China 3 Institute of Earth Sciences,Academia Sinica,Taipei 115,Taizvan,China 4 Department of Geosciences,National Taiwan University,Taipei 10617 Taiwan,China;Effect of stress ratio and friction coefficient on composite P wave radiation patterns[J];地球物理学报;2011-04
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