中国大陆板内各块体及褶皱带形变状态的联合反演研究

joint inversion method which is used to research the model of block movement and strain about strain status of drape zones is presented by this paper. According to multi-year GPS data and seismic moment tensor data of inner Chinese continent, the whole movement vectors, shortened velocity vectors of the drape zones and sliding rule between each block are researched, and their dynamics meaning is discussed. The below results can be obtained from this paper. The whole movement of Chinese continent is north-east direction. The detailed movement of west continent is north-north-east direction. However, of east continent is north-east-east direction. The quantitative values of movement of sub-plates or blocks in the west mainland approximately are from 28.5mm.a-1 to 3.2mm.a-1. And they are from 8.3mm.a-1 to 2.7mm.a-1 in the east continent. So the whole trend in the west continent has a big movement toward north, and in the east continent has a small movement toward south or southeast. The strain of west continent is far bigger than that of east, and the strain of southwest is bigger than that of the southeast. It is whole showed that India plate jostles toward north-east and the south-north zone has cutting and absorbing phenomena. The total characteristics and present-day trends of deformation of inland drape zones are basically described by the sinistrorse dislocation in south-north zone and Arjin fracture, the sinistrorse shear between south china and north china, etc.