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《Chinese Journal of Geophysics》 2005-02
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The recent state of stress in the central Qinghai-Tibet Plateau according to in-situ stress measurements

WU Man-Lu, ZHANG Chun-Shan, LIAO Chun-Ting, MA Yin-Sheng, OU Ming-Yi Institute of Geomechanics, Chinese Academy of Geological Science, Beijing 100081, China  
Qinghai-Tibet Plateau is most intensive in tectonic activity. In order to understand the recent state of stress, ground stress surveys were carried out at different structural positions and depths and in different rocks using piezomagnetic stress gauge overcoring method in the central Qinghai-Tibet Plateau. The results of stress measurements indicate that the direction of maximum principal stress is NE. This agrees with the result of the study of geology and earthquake and deformation. The values of maximum principal stress are 3.6~6.8MPa which are high as compared with those obtained elsewhere in China from a viewpoint of regional stress analysis. But the value and the direction of Amdo stress measurement site are different with those of other sites. The direction of maximum principal stress is NWW. The value of maximum principal stress is 8.1 MPa. This also indicates that the recent state of stress is complex near the plate suture zone. These results of stress measurements can provide important basic data as well for study of fault activity and geological hazard and engineering stability evaluation in Qinghai-Tibet railway, as also for continental dynamic study.
【Fund】: 国土资源部科技项目 (2 0 0 2 2 0 2 )资助
【CateGory Index】: P223;P542
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