South Yellow Seabasin can further be subdivided into northern depression, middle uplift zone and southern depression.
南黄海盆地进一步划分为北部坳陷、中部隆起区及南部坳陷。
2
Based on the structural geometry and kinematics of North Yellow Seabasin, the tectonic deformation style and geodynamic process of North Yellow Seabasin are studied.
以北黄海盆地构造几何学、运动学特征为基础，探讨了北黄海盆地的构造变形样式及动力学演化过程。
3
The natural geography of the Ordovician period is that: the Hannan paleocontinent and the Bashan Mountain rise at the north, and the wide epicontinental seabasin lies in the south.