KMS Nanjing Institute of Geology and Palaeonotology,CAS
The geometry and evolution of the deeply buried structural wedge in the kuqa fold-and-thrust belt: insights from numerical simulation | |
通讯作者 | Wang, Wei(wangw@nigpas.ac.cn) |
Chen, Weili1; Wang, Wei2; Zhao, Jiaqi1; Yin, Hongwei3; Hu, Fangjie1; Zhang, Yong2; Li, Zhihao1; Jia, Dong3; Zhang, Chunbo1 | |
2024-12-04 | |
发表期刊 | FRONTIERS IN EARTH SCIENCE |
卷号 | 12页码:19 |
摘要 | Numerical simulation is used to investigate the influence of thickness variation on the evolution of buried structural wedges, representing structures formed between two detachments. Simulations are based on the Kuqa fold-and-thrust belt, characterized by a tapered sedimentary sequence. Two sets of models were developed, one considering syn-tectonic sedimentation and the other without it. Model results indicate that an increase in thickness leads to larger intervals of thrusts, larger-scale thrust anticlines, and a reduced number of thrusts within the buried structural wedge, regardless of the presence of syn-tectonic sedimentation. The presence of syn-tectonic sedimentation is found to constrain the propagation of deformation within buried structural wedges, while increased thickness is observed to promote deformation propagation. Model results show that the deformation front expands toward the foreland from the thin model to the medium model and withdraws from the medium model to the thick model. This suggests that with the increase of wedge thickness, the restriction influence of syn-tectonic sedimentation on deformation propagation is more obvious than promotion. Model results show similarities in the structural features with the buried structural wedge in the Kuqa fold-and-thrust belt. With insights from numerical simulation, we suggest that the increased Mesozoic strata thickness from the west to east controls the structural variation along the strike. In the east, there are fewer thrust faults and larger fault intervals. Due to the restriction influence of the syn-tectonic sedimentation on the deformation propagation, the deformation front is an arc shape in the map view from west to east. |
关键词 | deformation propagation thickness variation numerical simulation kuqa depression structural wedges fold-and-thrust belts |
DOI | 10.3389/feart.2024.1494093 |
收录类别 | SCI |
语种 | 英语 |
关键词[WOS] | TIAN-SHAN MOUNTAINS ; TARIM BASIN ; SYNTECTONIC SEDIMENTATION ; OVERBURDEN THICKNESS ; TECTONIC EVOLUTION ; SALT STRUCTURES ; FORELAND BASIN ; WESTERN ; DEFORMATION ; EXAMPLE |
资助项目 | National Natural Science Foundation of China[41972219] ; National Natural Science Foundation of China[41572187] ; National Natural Science Foundation of China[42102270] ; National Natural Science Foundation of China[41927802] ; Fundamental Research Funds for NIGPAS[NGBS202422] |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:001379270500001 |
项目资助者 | National Natural Science Foundation of China ; Fundamental Research Funds for NIGPAS |
出版者 | FRONTIERS MEDIA SA |
文献类型 | 期刊论文 |
条目标识符 | http://ir.nigpas.ac.cn/handle/332004/44707 |
专题 | 中国科学院南京地质古生物研究所 |
通讯作者 | Wang, Wei |
作者单位 | 1.Tarim Oilfield Co, Res Inst Petr Explorat & Dev, Korla, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing, Peoples R China 3.Nanjing Univ, Sch Earth Sci & Engn, Nanjing, Peoples R China |
通讯作者单位 | 中国科学院南京地质古生物研究所 |
推荐引用方式 GB/T 7714 | Chen, Weili,Wang, Wei,Zhao, Jiaqi,et al. The geometry and evolution of the deeply buried structural wedge in the kuqa fold-and-thrust belt: insights from numerical simulation[J]. FRONTIERS IN EARTH SCIENCE,2024,12:19. |
APA | Chen, Weili.,Wang, Wei.,Zhao, Jiaqi.,Yin, Hongwei.,Hu, Fangjie.,...&Zhang, Chunbo.(2024).The geometry and evolution of the deeply buried structural wedge in the kuqa fold-and-thrust belt: insights from numerical simulation.FRONTIERS IN EARTH SCIENCE,12,19. |
MLA | Chen, Weili,et al."The geometry and evolution of the deeply buried structural wedge in the kuqa fold-and-thrust belt: insights from numerical simulation".FRONTIERS IN EARTH SCIENCE 12(2024):19. |
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