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《地球科学》 1994-06
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Evolution and Structural Style of Tianshan and Adjacent Basins, Northwestern China

Liu Hefu (Department of Energy Resources Geology, China University of Geosciences, Beijing 100083)Liang Huishe (Hebei College of Geology, Shijiazhuang 050031)Cai Liguo (Department of Energy Resources Geology, China University of Geosciences, Beijing 100083)Xia Yiping (Third Geophysical Survey Division, BGP, CNCP, Zhengding 050800)Liu Liqun (Institute of Petroleum Geology, MGMR, Beijing 100083)  
The Tianshan orogenic belt has a W-shape, composed of the V-shape Southern Tianshan and Northern Tianshan with different orogenic models. The Southern Tianshan broke off from the Sinian, forming a passive Continental margin and ocean, and closed during Silurian and Devonian. It belongs to the Wilson cycle orogenic model. The net duration is abo 400 Ma. The Northern Tianshan began back-are spreading during Devonian, forming the Devonian-Carboniferous marginal sea, and closed during Late Carboniferous. It belongs to the non-Wilson cycle orogenic model or back-are orogenic model. The duration is abo 100Ma. Deformation of the foreland fold -thrust belt occurred in two stages: in the early stage, folds and thrusts were formed by wedge - thrusting and lateral compression, while in the later stage, folds, gavitational normal faults and reverse faults were formed by the uplift of the Tianshan range and by gravity - gliding.
【Fund】: 国家自然科学基金项目(No.49712136)资助
【CateGory Index】: P542
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