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我国大部分地区的小新生代盆地的成生、演化受断裂构造的控制,泰和盆地即是严格受断裂构造控制的走滑拉张型盆地。本文着重从盆地的基底构造、盆缘断裂构造及盆地同生、后期构造阐述了它们与盆地形成和演化的关系。
The formation and evolution of the Little Cenozoic basins in most parts of China are controlled by fault structures. The Taihe Basin is a strike-slip extensional basin strictly controlled by fault structures. This paper focuses on the relationship between the basal structure, the basin margin fracture structure and the synsesis and the post-tectonic structure of the basin, and their relationship with the formation and evolution of the basin.