Multi-layer Tectonic Model for Intraplate Deformation and Plastic-Flow Network in the Asian Continental Lithosphere  

作　　者：Wang Shengzu Institute of Geology, State Seismological Bureau, Beijing Liu Linqun 

出　　处：《Acta Geologica Sinica(English Edition)》1993年第3期247-271,共25页地质学报（英文版）

基　　金：This project (No. 49070196) is funded by the National Science Foundation of China.

摘　　要：In a large area of the east—central Asian continent there is a unified seismic network system composed of two families of large—seismic belts that intersect conjugately. Such a seismic network in the middle—upper crust is actually a response to the plastic flow network in the lower lithosphere including the lower crust and lithospheric mantle. The existence of the unified plastic flow system confirms that the driving force for intraplate tectonic deformation results mainly from the compression of the India plate, while the long-range transmission of the force is carried out chiefly by means of plastic flow. The plastic flow network has a control over the intraplate tectonic deformation.In a large area of the east—central Asian continent there is a unified seismic network system composed of two families of large—seismic belts that intersect conjugately. Such a seismic network in the middle—upper crust is actually a response to the plastic flow network in the lower lithosphere including the lower crust and lithospheric mantle. The existence of the unified plastic flow system confirms that the driving force for intraplate tectonic deformation results mainly from the compression of the India plate, while the long-range transmission of the force is carried out chiefly by means of plastic flow. The plastic flow network has a control over the intraplate tectonic deformation.

关 键 词：Continental lithosphere tectonic deformation multi-layer tectonic model large-scale seismic belt seismic network plastic flow network 

分 类 号：P5[天文地球—地质学]