中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The geometry and evolution of the deeply buried structural wedge in the kuqa fold-and-thrust belt: insights from numerical simulation

文献类型:期刊论文

作者Chen, Weili1; Wang, Wei2; Zhao, Jiaqi1; Yin, Hongwei3; Hu, Fangjie1; Zhang, Yong2; Li, Zhihao1; Jia, Dong3; Zhang, Chunbo1
刊名FRONTIERS IN EARTH SCIENCE
出版日期2024-12-04
卷号12页码:19
关键词deformation propagation thickness variation numerical simulation kuqa depression structural wedges fold-and-thrust belts
DOI10.3389/feart.2024.1494093
通讯作者Wang, Wei(wangw@nigpas.ac.cn)
英文摘要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.
WOS关键词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
语种英语
WOS记录号WOS:001379270500001
出版者FRONTIERS MEDIA SA
资助机构National Natural Science Foundation of China ; Fundamental Research Funds for NIGPAS
源URL[http://ir.nigpas.ac.cn/handle/332004/44706]  
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
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.

入库方式: OAI收割

来源:南京地质古生物研究所

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