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《Earth Science(Journal of China University of Geosciences)》 2014-08
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Evolution of Sedimentary Basins in Tarim during Neoproterozoic-Paleozoic

Zou Yarui;Ta Jiguli;Xing Zuoyun;Xu Zenglian;Tang Tingting;Hao Yiwei;Institute of Geological Survey,China University of Geosciences;Faculty of Earth Sciences,China University of Geosciences;  
Tarim basin,located in southern Xinjiang Uygur Autonomous Region of Northwest China,held among the Tianshan,Kunlun and Altun fold belts,is a large,superimposed basin which has a long evolutional history.Based on the comprehensive study of the previous results,we conduct a comparative study of lithostragraphy and sedimentary,and divide the Tarim area into 8types of sedimentary basin during Neoproterozoic-Mesozoic,including passive continental margin,failed rift,carbonate platform,clastic epeiric sea,residual sea,mixed clastic-carbonate epeiric sea,inland graben basin,and foreland basin.The tectonic environments of basin formation and evolution are analyzed in this paper:Early Neoproterozoic,Tarim turned into stable stage of cover development.During Qingbaikouan,rift and passive continental margin were developed.Nanhua-Early Sinian,mortality rift and continental glaciers were developed.Carbonate platform,clastic epeiric sea and clastic-carbonate epeiric sea mainly developed during Paleozoic.The collision between Tarim and Kazakhstan-Junggar plate led to later subduction of the southern Tianshan oceanic basin of Carboniferous at the Late Carboniferous-Early Permian.At the beginning of Middle Permian,most of the Tarim evolved to foreland basin.
【Fund】: 中国地质调查局项目(No.1212010733802 12120113012500)
【CateGory Index】: P534
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