摘要
软流圈隆升是板块相互作用的深部调整过程，同时也是地壳表层—地幔进行重力均衡调整的过程。中国东部中新生代沉积盆地充填形态大多与盆地深部软流圈的隆升呈镜像对应关系，这一关系暗示了岩石圈和软流圈相互作用的耦合关系，也指示了伸展型盆地深部软流圈隆升幕的阶段性与盆地充填演化阶段之间的成因联系。
Asthenosphere uplift indicates the deep adjustment process during the interaction of plates, and also shows the adjusting process of gravitational equilibrium between upper layer of crust and mantle. It is the fact that the filling configuration of most of Meso Cenozoic basins shows a mirror image with the contour of asthenosphere uplift underneath the basins in East China. The results imply the coupling relationship resulted from the interaction of lithosphere and asthenosphere, and also reflect the genetic relationship between the uplifting episode of asthenosphere and the filling evolutionary stages of extending basins.
出处
《地学前缘》
EI
CAS
CSCD
1998年第A08期162-165,共4页
Earth Science Frontiers
基金
地质矿产部重大基础项目
