Keywords: 
• Dongting basin /
• Tenso-shear rift Basin /
• Basin-mountion coupling /
• Xuefeng-Mufu Orogenic belt

Abstract: According to the data of geology, physical geography, the structural physiognomy and so on, the style of the structure, the feature of the transmutation and formation between Dongting basin and Xuefeng -Mufu Orogenic belt are completely analyzed, it is considered that there is extreme coupling between the Orogenic belt and basins in the different periods of Meso-Cenozoic:1）The early and metaphase stage of Yansha（J₃—K_1-2），the resources of the study area is from the mountain around, the coupling of mountainbasin only indicates the filling and leveling up relation of the erosion of high area ,accumulation of low area. 2）The late stage of Yanshan（K_31-2），Due to the effect of the Pacific Ocean plate causing the sidelong nose down the  Eurasia plate in this period，Xuefeng-Mufu Orogenic belt was quickly uplifting and forming a series of fault blocks which controlled the development of Dongting basin along the extension-compression fault. The formation of Dongting basin and the stretching and sinking of later time of Xuefeng-Mufu Orogenic belt.3）The early stage of Himalayan movement（the late stage of the late Cretaceous to the Paleogene）the period of which Xuefeng-Mufu Orogenic belt the extension environment is the main reason that Dongting basin are extremely extention and transmutation, tenso-shear rift basin are more dustpan-shaped. 4）The late stage of Himalayan movement（Neogene-Quaternary）, the Xuefeng-Mufu Orogenic Belt since the main episode of the Himalayan movement in the Oligocene totally displaing weakly compressive and comresso-shear orogenic uplifting and being gradually denuded and leveled,and providing material sorces for the down-warped deposition of the Dongting Basin in the Neogene-Quaternary.