Tertiary evolution of the western Tarim basin, northwest China: A tectono-sedimentary response to northward indentation of the Pamir salient
文献类型：期刊论文
| 作者 | Wei, Hong-Hong1; Meng, Qing-Ren2; Ding, Lin1; Li, Zhen-Yu1 |
| 刊名 | TECTONICS
 |
| 出版日期 | 2013-06-01 |
| 卷号 | 32期号:3页码:558-575 |
| 关键词 | Western Tarim basin tertiary West Kunlun Shan Pamir tectonics sedimentation |
| DOI | 10.1002/tect.20046 |
| 文献子类 | Article |
| 英文摘要 | This paper deals with the Tertiary tectonic and sedimentary evolution of the western Tarim basin based on an integrated stratigraphic, sedimentary, structural, and tectonic analyses. Basin evolution is divided into three stages: Paleogene, Miocene, and Pliocene. The western Tarim basin was the easternmost part of the Tethyan realm from Late Cretaceous to Paleogene, and marine sedimentation continued into the Early Miocene. Miocene development of the western Tarim basin was chiefly governed by West Kunlun right-slip faulting and the simultaneous northward thrusting of the Pamir salient and Tianshuihai terrane. Yecheng subbasin developed as a pull-apart basin owing to synchronous activity of the West Kunlun and the Shache-Yangdaman right-slip faults. Hotan foreland basin formed in response to northward displacement of the Tianshuihai terrane, and another might have developed in front of the advancing Pamir salient in the Miocene. Basinward thrusting became predominant in the orogenic belts adjacent to the western Tarim basin in the Pliocene. North-directed displacement and uplift of the Tiklik thrust terrane fragmented the preexisting Hotan foreland basin, and collision of the Pamir with the southern Tian Shan deformational fronts caused complete destruction of the Miocene Pamir foreland basin. Eastward displacement of the Qimugen fold-thrust system led to flexural subsidence of the Yecheng subbasin in the Pliocene. Kashi subbasin developed as part of the southern Tian Shan foreland basin, and was controlled by the eastern Pamir as well. A tectonic scenario is proposed to illustrate complicated interplay of the western Tarim basin with its peripheral orogens in the Tertiary. |
| WOS关键词 | HIMALAYAN-TIBETAN OROGEN ; KARAKORAM FAULT ZONE ; CENTRAL-ASIA ; TIEN-SHAN ; TIAN-SHAN ; CENOZOIC DEFORMATION ; SEDIMENTARY BASINS ; FORELAND BASIN ; PLATEAU ; MARGIN |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000322124300016 |
| 资助机构 | National Science Foundation of China(41272238 ; National Science Foundation of China(41272238 ; 40721003 ; 40721003 ; 40972151) ; 40972151) ; National Science Foundation of China(41272238 ; National Science Foundation of China(41272238 ; 40721003 ; 40721003 ; 40972151) ; 40972151) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/62525]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Key Lab Continental Collis & Plateau Uplift, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China 2.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100101, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wei, Hong-Hong,Meng, Qing-Ren,Ding, Lin,et al. Tertiary evolution of the western Tarim basin, northwest China: A tectono-sedimentary response to northward indentation of the Pamir salient[J]. TECTONICS,2013,32(3):558-575. |
| APA | Wei, Hong-Hong,Meng, Qing-Ren,Ding, Lin,&Li, Zhen-Yu.(2013).Tertiary evolution of the western Tarim basin, northwest China: A tectono-sedimentary response to northward indentation of the Pamir salient.TECTONICS,32(3),558-575. |
| MLA | Wei, Hong-Hong,et al."Tertiary evolution of the western Tarim basin, northwest China: A tectono-sedimentary response to northward indentation of the Pamir salient".TECTONICS 32.3(2013):558-575. |
入库方式： OAI收割
来源：地质与地球物理研究所
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