supported by the National Key R&D Program of China (Grant Nos.2022YFF0800404,2022YFF0800402)。
The subduction and rollback of the paleo-Pacific plate during Mesozoic time was the key engine for the evolution of the continental margin in eastern China. It led to lateral accretion of continental crust in Northeas...
1.Current status Three-dimensional(3D)inversion of geophysical EM data is generally underdetermined,non-linear,and of large-scale that is very difficult to solve by optimization.In the past two decades,with the advanc...
supported by the National Natural Science Foundation of China(Grant Nos.41574093,41774114);SinoProbe-02(Grant No.A1011B)
Based on deep geophysical detections, we have reconstructed the crustal structure from the eastern margin of the Tibetan Plateau to the Jiangnan-Xuefeng orogenic belt. The results suggest that the Yangtze Block was ov...
supported by the National Natural Science Foundation of China(Grant No.40238060);the National Basic Research Program of China(Grant No.G20000467-02);the Key Project of the Chinese Academy of Sciences(Grant No.KZCX2-SW-117);the National Special Project(Grant No.2001DIA50041).
A segment of Mesozoic subduction-accretion zone was inferred across thenortheastern South China Sea at approximately NE450 orientation. Basic evidence includes thefollowing: A belt of peek gross horizontal Bouguer gra...
Project supported by the National Natural Science Foundation of China
Based on the analysis of the 1993 and 1995 GPS data acquired from crust movement and deformationmonitoring in the Qinghai-Xizang Plateau, the following preliminary conclusions could be drawn: the levelly movingrate an...
Project supported by National "Eighth Five-Year" Climbing Project.
Comprehensive investigations along the Gyirong-Lugu-Sangehu geophysical profile in the western Xizang Plateau are presented. Analysis and interpretation of the lithospheric structure resulted in setting up of the geop...