The 1°×1° distribution map of crustmantle structural ratio R for the lithosphere along the Longitudinal Seismic Belt of China has been compiled using computer based on the results of geophysical prospec...The 1°×1° distribution map of crustmantle structural ratio R for the lithosphere along the Longitudinal Seismic Belt of China has been compiled using computer based on the results of geophysical prospecting by previous researchers, and the latest results by the present authors. Based on this map, an insight into the structural features of the crustmantle assemblage along the Longitudinal Seismic Belt has been gained, while their relation to seismic activity and the distributions of geothermal flux and intracrustal high conductivitylow velocity layers, as well as their tectonic effect to seismicity have been discussed.展开更多
An enigmatic feature of Precambrian continental lithosphere is its long-term stability,which depends on the degree of coupling between the crust and mantle since cratonisation.Earlier studies infer deformation of the ...An enigmatic feature of Precambrian continental lithosphere is its long-term stability,which depends on the degree of coupling between the crust and mantle since cratonisation.Earlier studies infer deformation of the lower lithosphere by mantle flow with fast direction of seismic anisotropy being parallel to present plate motion.展开更多
文摘The 1°×1° distribution map of crustmantle structural ratio R for the lithosphere along the Longitudinal Seismic Belt of China has been compiled using computer based on the results of geophysical prospecting by previous researchers, and the latest results by the present authors. Based on this map, an insight into the structural features of the crustmantle assemblage along the Longitudinal Seismic Belt has been gained, while their relation to seismic activity and the distributions of geothermal flux and intracrustal high conductivitylow velocity layers, as well as their tectonic effect to seismicity have been discussed.
基金supported by grants FNU10-083081 to IMA and FNU11-104254 to HT from the Danish Research Councilthe MOST funds for GPMR State Key Laboratory(CUG-Wuhan)(GPMR2019010)
文摘An enigmatic feature of Precambrian continental lithosphere is its long-term stability,which depends on the degree of coupling between the crust and mantle since cratonisation.Earlier studies infer deformation of the lower lithosphere by mantle flow with fast direction of seismic anisotropy being parallel to present plate motion.
