On the basis of synthetic studies of geology, geophysics and geochemistry, the present Qinling Orogenic Belt can be described as a 3-D "flyover-type" geometric model with rheological layering structures. Fur...On the basis of synthetic studies of geology, geophysics and geochemistry, the present Qinling Orogenic Belt can be described as a 3-D "flyover-type" geometric model with rheological layering structures. Furthermore, the tectonic dynamic analyses have been done based on the structural geometry and kinematic features. Thus it can be concluded that its present structure has resulted from an adjustment of deep-seated mantle dynamics and lithosphere coupling relationship since the Mesozoic-Cenozoic time.展开更多
基金Project supported by the National Natural Science Foundation of China.
文摘On the basis of synthetic studies of geology, geophysics and geochemistry, the present Qinling Orogenic Belt can be described as a 3-D "flyover-type" geometric model with rheological layering structures. Furthermore, the tectonic dynamic analyses have been done based on the structural geometry and kinematic features. Thus it can be concluded that its present structure has resulted from an adjustment of deep-seated mantle dynamics and lithosphere coupling relationship since the Mesozoic-Cenozoic time.
