supported by the Natural Science Foundation of China (No. 40674026);Commonweal Special Science Foundation of China (Grant No. 200811037)
This paper analyzes various earthquake fault types, mechanism solutions, stress field as well as other geophysical data to study the crust movement in the Tibetan plateau and its tectonic implications. The results sho...
supported partly by National Natural Science Foundation of China(No.40674026);Commonweal Special Science Foundation of China(No.200811037);Geological Survey Foundation of Ministry of Land and Resource,China(No.1212010916083)
In the present analysis on the relationships among the depth of lithosphere brittle fracture, seismotectonics and geothermal anomalous active in Tibetan plateau were investigated using the seismic dada from ISC and Ch...
supported by the National Natural Science Foundation of China (No. 40674026)
Various earthquake fault types, mechanism solutions, stress field, and other geophysical data were analyzed for study on the crust movement in the Tibetan plateau and its tectonic implications. The results show that n...
supported financially by the National Natural Science Foundation of China (No. 40674026)
Various earthquake fault types were analyzed for this study on the crust movement in the high region of the Tibetan plateau by analyzing mechanism solutions and stress fields. The results show that a lot of normal fau...
Supported partly by National Natural Science Foundation of China (Grant No.40674026);National Special Science Foundation of China (Grant No.200811037)
The 3-D crustal structure of P-wave velocity in East China is studied based on the data obtained by wide-angle seismic reflection and refraction surveys.The results suggest that a deep Moho disconti-nuity exists in th...