塔里木新元古代-古生代沉积盆地演化

邹亚锐; 塔吉古丽; 邢作云; 徐增连; 唐婷婷; 郝奕玮

doi:10.3799/dqkx.2014.104

Volume 39 Issue 8

Aug. 2014

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Article Navigation > Earth Science > 2014 > 39(8): 1200-1216

Zou Yarui, Ta Jiguli, Xing Zuoyun, Xu Zenglian, Tang Tingting, Hao Yiwei, 2014. Evolution of Sedimentary Basins in Tarim during Neoproterozoic-Paleozoic. Earth Science, 39(8): 1200-1216. doi: 10.3799/dqkx.2014.104

Citation:

Zou Yarui, Ta Jiguli, Xing Zuoyun, Xu Zenglian, Tang Tingting, Hao Yiwei, 2014. Evolution of Sedimentary Basins in Tarim during Neoproterozoic-Paleozoic. Earth Science, 39(8): 1200-1216. doi: 10.3799/dqkx.2014.104

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Evolution of Sedimentary Basins in Tarim during Neoproterozoic-Paleozoic

doi: 10.3799/dqkx.2014.104

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2014-03-12
Publish Date: 2014-08-01

Abstract

Abstract

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 8 types 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.
- Tarim basin,
- sedimentology,
- tectonics,
- evolution

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References(178)

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