The evolution of a strike-slip fault network in the Guchengxu High, Tarim Basin (NW China)
文献类型：期刊论文
| 作者 | Qiu, Huabiao2; Deng, Shang2; Zhang, Jibiao2; Lin, Huixi2; Huang, Cheng1; Han, Jun1; Lin, Wei4; Zhu, Xin3 |
| 刊名 | MARINE AND PETROLEUM GEOLOGY
 |
| 出版日期 | 2022-06-01 |
| 卷号 | 140页码:16 |
| 关键词 | Tectonic responses Sequential evolution Strike-slip fault network Guchengxu high Tarim basin |
| ISSN号 | 0264-8172 |
| DOI | 10.1016/j.marpetgeo.2022.105655 |
| 英文摘要 | Convergent plate margins could have an immediate impact on intraplate deformation in the adjacent sedimentary basin. In the Tarim Basin, a strike-slip fault network in the Guchengxu High is adjacent to the Tethys (northern Tibetan Plateau). This paper uses high-quality 3-D seismic data to unravel the geometry and kinematics of the strike-slip fault network and the genetic relationship with the Tethys tectonics. Within the fault network, the left-lateral NNE-and ENE-oriented strike-slip faults are a result of sequential evolution rather than conjugate faults. The sub-vertical ENE-oriented strike-slip faults are widely spaced with stepping-segmented geometry in the west, whereas they are relatively clustered with larger vertical throws close to the Cherchen fault. They were interpreted as a series of the Cherchen fault-related structures due to oblique blocking of the Tazhong Uplift and block deflection. It responded to the Late Ordovician Altyn Tagh/Tarim collisional orogeny and the Cherchen fault. The NNE-oriented strike-slip faults are characterized by underlying sub-vertical faults and two layers of overlying normal faults. These NNE-oriented strike-slip faults have large transversal compressional components, commonly presenting reverse drags on both sides of the underlying sub-vertical faults. These NNE-oriented faults initiated on pre-existing discontinuities (extensional joints) and offset the ENE-oriented ones when NNW-oriented stress was transmitted to plate interiors during this Late Ordovician orogeny. Afterward, two layers of overlying normal faults formed due to dragging of the covers during the Middle Silurian-Early Carboniferous reactivation and the Late Carboniferous-Early Permian inversion, in response to subduction of the Kunlun Ocean and opening of the Paleo-Tethys Ocean, respectively. The strike-slip fault network in plate interiors evolved as immediate responses to the Tethys tectonics at plate boundaries. |
| WOS关键词 | ALTYN-TAGH FAULT ; NORTHERN TIBETAN PLATEAU ; TECTONIC EVOLUTION ; TAZHONG UPLIFT ; OROGENIC BELT ; DISPLACEMENT ; CONSTRAINTS ; GEOMETRY ; RECONSTRUCTIONS ; PALEOGEOGRAPHY |
| 资助项目 | Joint Funds of the National Natural Science Foundation of China[U21B2063] ; Joint Funds of the National Natural Science Foundation of China[U19B6003] ; Northwest Oilfield Company (SINOPEC) |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000805223800001 |
| 出版者 | ELSEVIER SCI LTD |
| 资助机构 | Joint Funds of the National Natural Science Foundation of China ; Joint Funds of the National Natural Science Foundation of China ; Northwest Oilfield Company (SINOPEC) ; Northwest Oilfield Company (SINOPEC) ; Joint Funds of the National Natural Science Foundation of China ; Joint Funds of the National Natural Science Foundation of China ; Northwest Oilfield Company (SINOPEC) ; Northwest Oilfield Company (SINOPEC) ; Joint Funds of the National Natural Science Foundation of China ; Joint Funds of the National Natural Science Foundation of China ; Northwest Oilfield Company (SINOPEC) ; Northwest Oilfield Company (SINOPEC) ; Joint Funds of the National Natural Science Foundation of China ; Joint Funds of the National Natural Science Foundation of China ; Northwest Oilfield Company (SINOPEC) ; Northwest Oilfield Company (SINOPEC) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/105975]  |
| 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.SINOPEC Northwest Oilfield Co, Explorat & Prod Res Inst, Urumqi 830011, Xinjiang, Peoples R China 2.SINOPEC, Petr Explorat & Prod Res Inst, Beijing 100083, Peoples R China 3.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Shanxi, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Qiu, Huabiao,Deng, Shang,Zhang, Jibiao,et al. The evolution of a strike-slip fault network in the Guchengxu High, Tarim Basin (NW China)[J]. MARINE AND PETROLEUM GEOLOGY,2022,140:16. |
| APA | Qiu, Huabiao.,Deng, Shang.,Zhang, Jibiao.,Lin, Huixi.,Huang, Cheng.,...&Zhu, Xin.(2022).The evolution of a strike-slip fault network in the Guchengxu High, Tarim Basin (NW China).MARINE AND PETROLEUM GEOLOGY,140,16. |
| MLA | Qiu, Huabiao,et al."The evolution of a strike-slip fault network in the Guchengxu High, Tarim Basin (NW China)".MARINE AND PETROLEUM GEOLOGY 140(2022):16. |
入库方式： OAI收割
来源：地质与地球物理研究所
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