利用南襄盆地的深部地球物理测深成果资料,简述盆地深部地质结构与构造特征,从系统论出发,讨论了盆地的岩石圈结构和盆地的深部过程及盆地成因动力学条件,进而探讨了岩石圈介质的构造成层和构造-热结构对盆地油气生成与运移的控制作用。认为盆地相对造山带而言,软流圈浅埋和“薄慢薄壳”,深部过程以岩石圈塑性形变和岩石圈伸展-热均衡为主,盆地相侧向分块、垂向解耦和塑性高温对油气的生成和运移起控制作用。 Based on the deep geophysical sounding data of Nanxiang Basin, the deep geological structure and tectonic features of the basin are briefly described. Based on the systematic theory, the lithosphere structure of the basin and the deep process of the basin and the genesis kinetic conditions of the basin are discussed. Structural stratigraphy and tectono - lithosphere media controlling the formation and migration of oil and gas in the basin. In terms of relative orogen, the shallow asthenosphere and “thin and slow shell” in the basin are dominated by plastic deformation of the lithosphere and extension of the lithosphere-thermal equilibrium. The basin is laterally subdivided and decoupled vertically Plastic high temperature can control the formation and migration of oil and gas.