Dependence of Coseismic Landslide Distribution Patterns on Fault Movement
文献类型:期刊论文
| 作者 | Li, Wenping2,3,4; Wu, Yuming2; Gao, Xing2; Wang, Weimin1 |
| 刊名 | APPLIED SCIENCES-BASEL
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| 出版日期 | 2025-09-23 |
| 卷号 | 15期号:19页码:10305 |
| 关键词 | coseismic landslides fault type large earthquakes ground motion distribution pattern frequency-area distribution |
| DOI | 10.3390/app151910305 |
| 产权排序 | 2 |
| 文献子类 | Article |
| 英文摘要 | Faults are the primary drivers of earthquakes and exert a strong control on rupture mechanisms, earthquake magnitude, and the spatial distribution of coseismic landslides (CLs). However, how CL spatial distribution patterns vary with faulting style remains poorly constrained. Here, we compiled a catalog of CLs associated with 18 global major earthquakes (M-W > 6.0) within continental regions since 1900 and explored the distribution patterns of CLs associated with the three major earthquake types: oblique-slip, dip-slip, and strike-slip. Our results reveal two distinct spatial distribution patterns of CLs: a hanging-wall distribution for oblique-slip and dip-slip earthquakes and a bell-shaped distribution for strike-slip earthquakes. The orientation of CLs is closely related to fault geometry and slip type. Specifically, in oblique-slip, strike-slip, and dip-slip earthquakes, CLs predominantly develop parallel, perpendicular, or perpendicular to the fault strike, respectively. In terms of slip rake, CLs are mainly aligned perpendicular, parallel, and parallel to the fault slip direction for oblique-slip, strike-slip, and dip-slip events, respectively. Importantly, the distribution patterns of CLs encode information about ground movement during an earthquake. While Peak Ground Acceleration (PGA) serves as an indicator of ground motion intensity, a comprehensive characterization of CLs-including their size and predominant movement direction-requires consideration of both the earthquake type and the local slope conditions. |
| URL标识 | 查看原文 |
| WOS关键词 | EARTHQUAKE-INDUCED LANDSLIDES ; CHI-CHI EARTHQUAKE ; 2008 WENCHUAN EARTHQUAKE ; RUPTURE PROCESS ; STRONG-MOTION ; SPATIAL-DISTRIBUTION ; COMPLEX RUPTURE ; 1994 NORTHRIDGE ; SLIP HISTORY ; HANGING WALL |
| WOS研究方向 | Chemistry ; Engineering ; Materials Science ; Physics |
| 语种 | 英语 |
| WOS记录号 | WOS:001594588000001 |
| 出版者 | MDPI |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/217545] ![]() |
| 专题 | 资源与环境信息系统国家重点实验室_外文论文 |
| 通讯作者 | Wu, Yuming |
| 作者单位 | 1.Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China 2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, State Key Lab Resources & Environm Informat Syst, Beijing 100101, Peoples R China; 3.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China; 4.Shanghai Inst Tourism, Digital Technol & Innovat Res Ctr Culture & Touris, Shanghai 201418, Peoples R China; |
| 推荐引用方式 GB/T 7714 | Li, Wenping,Wu, Yuming,Gao, Xing,et al. Dependence of Coseismic Landslide Distribution Patterns on Fault Movement[J]. APPLIED SCIENCES-BASEL,2025,15(19):10305. |
| APA | Li, Wenping,Wu, Yuming,Gao, Xing,&Wang, Weimin.(2025).Dependence of Coseismic Landslide Distribution Patterns on Fault Movement.APPLIED SCIENCES-BASEL,15(19),10305. |
| MLA | Li, Wenping,et al."Dependence of Coseismic Landslide Distribution Patterns on Fault Movement".APPLIED SCIENCES-BASEL 15.19(2025):10305. |
入库方式: OAI收割
来源:地理科学与资源研究所
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