| 沉积盆地形成的地球动力学机制及其分类 |
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| 引用本文： | 王东坡,刘立,薛林福,杨光,许敏,王骏,王德勤.沉积盆地形成的地球动力学机制及其分类[J].沉积与特提斯地质,1998,18(3):7-13. |
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| 作者姓名： | 王东坡 刘立 薛林福 杨光 许敏 王骏 王德勤 |
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| 作者单位： | 长春科技大学长春，王氏有限公司 |
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| 摘 要： | 沉积盆地的形成主要与地球内部的热和物质的对流密切相关，它是沉积盆地形成和演化的原始动力。软流圈上涌高谋划在面或地幔羽的位置是地幔对 具体的表现。
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| 关 键 词： | 地幔对流 流变学界限 地球动力学 沉积盆地 |
Geodynamic mechanisms for the formation of sedimentary basins and their classification |
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| Wang Dongpo,Liu Li,Xue Linfu,Yang Guang,Xu Min,Wang Jun,Wang Deqin.Geodynamic mechanisms for the formation of sedimentary basins and their classification[J].Sedimentary Geology and Tethyan Geology,1998,18(3):7-13. |
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| Authors: | Wang Dongpo Liu Li Xue Linfu Yang Guang Xu Min Wang Jun Wang Deqin |
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| Institution: | 1 Changchun University of Science and Technology;2 D. C. Wang Inc. Boise ID, 83725, U. S. A |
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| Abstract: | The formation of sedimentary basins is considered to be closely related to the thermal and material convection in the Earth''s interior.The mantle convection is the primary driv-ing force for the formation and evolution of sedimentary basins,and manifested in the posi-tion of the asthenosphere,Moho discontinuity and mantle plume.The ancestrial basins have been classified,in this paper,into cratonic,extensional,compressional and strike-slip basins according to the rheologic boundary within the mantle lithosphere,the nature and thickness of the lithospere,intraplate stress,and sedimentary loading. |
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| Keywords: | mantle convection rheologic boundary nature of the lithosphere intraplate stress sedimentary loading |
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