The Evolution of the Complex Anticlinal Belt With Crosscutting Strike-Slip Faults in the Central Tarim Basin, NW China
文献类型：期刊论文
| 作者 | Qiu, Huabiao1,2,3; Deng, Shang2,4; Cao, Zicheng2; Yin, Ting2; Zhang, Zhongpei4 |
| 刊名 | TECTONICS
 |
| 出版日期 | 2019-06-01 |
| 卷号 | 38期号:6页码:2087-2113 |
| 关键词 | tectonic evolution the complex anticlinal belt strike-slip faults the central Tarim Basin basinal response the Proto-Tethys tectonics |
| ISSN号 | 0278-7407 |
| DOI | 10.1029/2018TC005229 |
| 英文摘要 | Integrated 2-D and 3-D seismic data sets reveal that a WNW trending complex anticlinal belt (the Tazhong Uplift) was cut roughly perpendicularly by a series of NNE oriented strike-slip faults in the central Tarim Basin, NW China. Through detailed interpretation of the internal architecture of the Tazhong Uplift and the structural characteristics of the strike-slip faults, the timing of their movements was determined. Based upon their geometric relationship and coeval movement, we propose an integrated model for the evolution of both the Tazhong Uplift and the strike-slip fault system. Initially, the Tazhong Uplift formed perpendicular to the NNE oriented compression that responded to the collision between the Tarim block and the western Kunlun terrane in the latest Middle Ordovician. Meanwhile, regional joints formed parallel to the maximum compression, that is, perpendicular to the Tazhong Uplift. In the latest Ordovician, northward compression caused the uplifting climax of the Tazhong Uplift in response to the collision between the Tarim block and the coherent eastern Kunlun-Altyn Tagh-Qaidam-Qilian terrane. Under such a northward compression, the resolved shear stress on the NNE trending joints formed the transpressional strike-slip faults. Afterward, the Tazhong Uplift tilted northward during the ongoing subduction from the Kunlun Ocean, which lasted until the latest Middle Devonian. The negative flower structures formed along the preexisting transpressional strike-slip faults due to the dragging of the overlying covers in the latest Middle Devonian. The data and evolution model not only unveil the formation mechanism of the Tazhong Uplift and the associated strike-slip faults but also provide further constraints on the evolutionary age of the Proto-Tethys Ocean. |
| WOS关键词 | ALTYN-TAGH FAULT ; NORTHERN TIBET IMPLICATIONS ; KUNLUN OROGENIC BELT ; WESTERN KUNLUN ; TECTONIC EVOLUTION ; TAZHONG UPLIFT ; HYDROCARBON ACCUMULATIONS ; ACCRETIONARY TECTONICS ; CHARGE HISTORY ; TIEN-SHAN |
| 资助项目 | NSFC[91855212] ; NSFC[91755205] ; NSFC[41472193] ; NSTMP of China[2017ZX05005] ; National Key R&D Program of China[2016YFC0600401] ; National Key R&D Program of China[2016YFC0600102] ; Sinopec Group, Department of Technology, Geosciences Basic Research Program[P17045-5] ; Sinopec Group, Department of Technology, Geosciences Basic Research Program[G5800-17-ZS-KJB047] |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000475363100012 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 资助机构 | NSFC ; NSFC ; NSTMP of China ; NSTMP of China ; National Key R&D Program of China ; National Key R&D Program of China ; Sinopec Group, Department of Technology, Geosciences Basic Research Program ; Sinopec Group, Department of Technology, Geosciences Basic Research Program ; NSFC ; NSFC ; NSTMP of China ; NSTMP of China ; National Key R&D Program of China ; National Key R&D Program of China ; Sinopec Group, Department of Technology, Geosciences Basic Research Program ; Sinopec Group, Department of Technology, Geosciences Basic Research Program ; NSFC ; NSFC ; NSTMP of China ; NSTMP of China ; National Key R&D Program of China ; National Key R&D Program of China ; Sinopec Group, Department of Technology, Geosciences Basic Research Program ; Sinopec Group, Department of Technology, Geosciences Basic Research Program ; NSFC ; NSFC ; NSTMP of China ; NSTMP of China ; National Key R&D Program of China ; National Key R&D Program of China ; Sinopec Group, Department of Technology, Geosciences Basic Research Program ; Sinopec Group, Department of Technology, Geosciences Basic Research Program |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/92666]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 通讯作者 | Qiu, Huabiao; Deng, Shang |
| 作者单位 | 1.Chinese Acad Sci, Inst Earth Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 2.Explorat & Dev Res Inst, SINOPEC Northwest Oilfield Branch, Urumqi, Peoples R China 3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China 4.SINOPEC, Petr Explorat & Prod Res Inst, Beijing, Peoples R China |
| 推荐引用方式 GB/T 7714 | Qiu, Huabiao,Deng, Shang,Cao, Zicheng,et al. The Evolution of the Complex Anticlinal Belt With Crosscutting Strike-Slip Faults in the Central Tarim Basin, NW China[J]. TECTONICS,2019,38(6):2087-2113. |
| APA | Qiu, Huabiao,Deng, Shang,Cao, Zicheng,Yin, Ting,&Zhang, Zhongpei.(2019).The Evolution of the Complex Anticlinal Belt With Crosscutting Strike-Slip Faults in the Central Tarim Basin, NW China.TECTONICS,38(6),2087-2113. |
| MLA | Qiu, Huabiao,et al."The Evolution of the Complex Anticlinal Belt With Crosscutting Strike-Slip Faults in the Central Tarim Basin, NW China".TECTONICS 38.6(2019):2087-2113. |
入库方式： OAI收割
来源：地质与地球物理研究所
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