ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
昆仑山与汶川强烈地震对青藏块体东北缘地壳运动及应变积累的影响
  
关键词:the Ms8.1 Kunlun Mountains earthquake  the Ms8.0 Wenchuan earthquake  northeastern margin of Xinghai-Xizang block  crustal movement  influence of great earthquakes
基金项目:“十一五”国家科技支撑项目(编号: 2006BAC01B02-02-03)与自然科学基金项目(编号: 40674010)
作者单位E-mail
张希 中国地震局第二监测中心 zxivy@yahoo.com.cn 
王双绪 中国地震局第二监测中心  
张晓亮 中国地震局第二监测中心  
崔笃信 中国地震局第二监测中心  
王文萍 中国地震局第二监测中心  
张四新 中国地震局第二监测中心  
薛富平 中国地震局第二监测中心  
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摘要:
The Influence of the Kunlun Mountains and Wenchuan StrongEarthquakes on the Crustal Movement and Strain Accumulationin the Northeastern Margin of Qinghai-Xizang Block
      Making full use of crustal deformation data obtained from GPS, regional leveling and cross-fault means, aided by the inversion of negative dislocation, and combined with seismic activities, the authors studied the influence of the Ms8.1 Kunlun Mountains Great Earthquake of November 14, 2001 on the crustal movement and strain accumulation in the northeastern margin of Qinghai-Xizang block. The result shows that it was the adjustment ac-tion of disturbance stress field caused by this enormous seismic energy releasing inside Qinghai-Xizang block in the northeastward compressional background field that led to the variation of the crustal difference movement and the stress-strain state in the block boundary. To some extent and for a period of time, the action mainly found ex-pression in the reduction of strain accumulation in the eastern segment of the Altyn Tagh fault and the western segment of the Qilian Mountain fracture zone, and in the promotion of strain accumulation in the middle-eastern segments of the Qilian Mountain fracture zone. Presently the regional stress field of the study area reflects the re-covering state after the Kunlun Mountains, Yumen and Minle earthquakes. Moreover, based on limited data ob-tained from GPS, short-leveling and cross-fault means after the Wenchuan Earthquake of May 12, 2008, the au-thors consider that the Wenchuan Earthquake promoted the strain accumulation in the eastern segment of the Gansu-Sichuan boundary as well as along the Gansu-Sichuan-Shaanxi boundary.
ZHANG Xi,WANG Shuang-xu,ZHANG Xiao-liang,CUI Du-xin,WANG Wen-ping,ZHANG Si-xin,XUE Fu-ping.2010.The Influence of the Kunlun Mountains and Wenchuan StrongEarthquakes on the Crustal Movement and Strain Accumulationin the Northeastern Margin of Qinghai-Xizang Block[J].Acta Geoscientica Sinica,31(1):32-42.
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