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- W2376674591 abstract "Cenozoic basins, widespread in theeontinent and marginal seas of East China, are main oil—controlling structures They are intermontane basins filled with molassoid formations consisting mainly of continental red beds. All of the basins are extensional basins. Some of them are rifts. They trend NNE to NNE, and are distributed in an eu echelon pattern, It is quite evident that they have resulted from a secondary tensile stress derived from a pair of dextral shear stresses. The evolutionary history of the lithosphere in East China shows that these basins formed in the late period of the development of the diwa regions from the activation and disintegration of the Chinese ancient platform, that is, after the major episode of the post-platform orogeny. At that period, heat flow relatively deereased and the crust relatively contracts. As a result, tension or tension-shear fraetures(or older non-tension fractures evolved into such fraetures)and extensional basins developed. Furthermore, spaeeborne gravimetric data show that mantle creeps southward under the western Pacific Ocean and northward urder southwest China and India. The N-S or sub N-S directed dextral shear stress created by the mantle creeping eurrents draws the corresponding parts of the crust, causes them to move in the same direction and prodnees another dextral shear stress. This determines the en echelon distribution and trend of the basins" @default.
- W2376674591 created "2016-06-24" @default.
- W2376674591 creator A5079834077 @default.
- W2376674591 date "1988-01-01" @default.
- W2376674591 modified "2023-09-28" @default.
- W2376674591 title "AN EXPLANATION ON THE ORIGIN-MECHANISM OF FORMATION OF THE CENOZOIC BASINS IN THE POST-PLATFORM OROGENIC BELTS OF EAST CHINA" @default.
- W2376674591 hasPublicationYear "1988" @default.
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