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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 2000-04
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THE TECTONIC-SEDIMENTARY FEATURE AND EVOLUTION OF QIANGTANG BASIN IN NORTHERN TIBET

HE Zhong_hua 1, LI Cai 1, YANG De_ming 1, CHEN Guang_quan 2 (1.Changchun University of Science and Technology, Changchun 130026, China; 2.Liaohe Petroleum Exploration Bureau, Panjin 124010,China)  
Qiangtang basin is a marine composite basin of Tethys domain in Tibet during late Paleozoic-Mesozoic period. It underwent three major stages (the late Paleozoic plate tectonic evoloution, Mesozoic plate tectonic evolution and Cenzoic uplift-denudation) and formed different basins, including continental margin basin in late Paleozoic, southern Qiangtang passive continental margin basin and northern Qiangtang back-arc basin in the Mesozoic, and tectonic-morphologic basin after late Jurassic. By the effict of multitectonic movements, from north to south Qiangtang basin can be divided into five tectonic units:northern margin thrust-fold belt, northern Qiangtang deformation belt, central collisional uplift belt, southern Qiangtang deformation belt and southern thrust-fault belt. The deformation is weaker from depression margin to centre. Jura-type fold style shows that the deofmation of covering strata is a kind of decollement in shallow level.
【Fund】: 中国石油天然气集团公司“九五”科技工程资助项目!(QZ-97-204102)
【CateGory Index】: P618.13
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