Topographic changes due to the 2008 Mw 7.9 Wenchuan earthquake as revealed by the differential DEM method

doi:10.1016/j.geomorph.2014.04.020

	Topographic changes due to the 2008 Mw 7.9 Wenchuan earthquake as revealed by the differential DEM method
	Ren, Zhikun 1,2; Zhang, Zhuqi 1; Dai, Fuchu 3; Yin, Jinhui 1; Zhang, Huiping 1
刊名	GEOMORPHOLOGY
	2014-07-15
卷号	217 页码:122-130
关键词	Wenchuan earthquake Longmen Shan Topographic change Denudation Differential DEM
ISSN号	0169-555X
DOI	10.1016/j.geomorph.2014.04.020
文献子类	Article
英文摘要	Landscape evolution in active orogenic regions is inevitably affected by the repeated strong earthquakes triggered by the corresponding active faults. However, the lack of adequate methods for the documentation and monitoring of mountain-building processes has resulted in a shortage of quantitative estimates of orogenic and eroded volumes. A strong earthquake and its associated co-seismic landslides represent a sudden pulse in landscape evolution in tectonically active areas. The 2008 Mw 7.9 Wenchuan earthquake dramatically modified the topography of the Longmen Shan region. Based on topographic data before the earthquake and stereo pairs of post-earthquake remote sensing imagery, we derived pre- and post-earthquake DEMs (digital elevation models) of the three regions along the Longmen Shan Thrust Belt. By comparing the geomorphic features before and after the earthquake, we find that the Wenchuan earthquake smoothed the steep relief and caused a co-seismic uplift of the Longmen Shan region. The medium-relief regions increased; however, the high-relief regions decreased, indicating that the local relief is controlled by repeated strong earthquakes. The changed slope aspect indicates that the formation and modification of the east- and west-facing slopes are controlled by tectonic events in the Longmen Shan region, which might be associated with the regional stress field. However, the unchanged aspects of other slopes might be controlled by long-term erosion rather than tectonic events. The topographic changes, landslide volume and co-seismic uplift indicate that the greatest seismically induced denudation occurred in association with a thrust faulting mechanism and low-angle fault geometry. Our findings reveal that the local relief has been shaped by the localized, seismically induced high rate of denudation within the plateau margins, and that the formation of local relief is also related to tectonic events, especially the events that have occurred on low-angle faults. This study also indicates that the multi-temporal DEM differential method is valuable in detecting seismically induced topographic change. (C) 2014 Elsevier B.V. All rights reserved.
WOS关键词	TIBETAN PLATEAU ; EASTERN MARGIN ; AIRBORNE LIDAR ; THRUST BELT ; CHINA ; EROSION ; LANDSLIDES ; FAULT ; SLIP ; DEFORMATION
WOS研究方向	Physical Geography ; Geology
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000338818700010
资助机构	National Natural Science Foundation of China(41102136 ; National Natural Science Foundation of China(41102136 ; Public Service Funds for Earthquake Studies(201308012) ; Public Service Funds for Earthquake Studies(201308012) ; National Nonprofit Fundamental Research Grant of China(IGCEA1119 ; National Nonprofit Fundamental Research Grant of China(IGCEA1119 ; Foundation of Returned Overseas Scholars of China ; Foundation of Returned Overseas Scholars of China ; 41372220 ; 41372220 ; IGCEA1220) ; IGCEA1220) ; 41304073) ; 41304073) ; National Natural Science Foundation of China(41102136 ; National Natural Science Foundation of China(41102136 ; Public Service Funds for Earthquake Studies(201308012) ; Public Service Funds for Earthquake Studies(201308012) ; National Nonprofit Fundamental Research Grant of China(IGCEA1119 ; National Nonprofit Fundamental Research Grant of China(IGCEA1119 ; Foundation of Returned Overseas Scholars of China ; Foundation of Returned Overseas Scholars of China ; 41372220 ; 41372220 ; IGCEA1220) ; IGCEA1220) ; 41304073) ; 41304073) ; National Natural Science Foundation of China(41102136 ; National Natural Science Foundation of China(41102136 ; Public Service Funds for Earthquake Studies(201308012) ; Public Service Funds for Earthquake Studies(201308012) ; National Nonprofit Fundamental Research Grant of China(IGCEA1119 ; National Nonprofit Fundamental Research Grant of China(IGCEA1119 ; Foundation of Returned Overseas Scholars of China ; Foundation of Returned Overseas Scholars of China ; 41372220 ; 41372220 ; IGCEA1220) ; IGCEA1220) ; 41304073) ; 41304073) ; National Natural Science Foundation of China(41102136 ; National Natural Science Foundation of China(41102136 ; Public Service Funds for Earthquake Studies(201308012) ; Public Service Funds for Earthquake Studies(201308012) ; National Nonprofit Fundamental Research Grant of China(IGCEA1119 ; National Nonprofit Fundamental Research Grant of China(IGCEA1119 ; Foundation of Returned Overseas Scholars of China ; Foundation of Returned Overseas Scholars of China ; 41372220 ; 41372220 ; IGCEA1220) ; IGCEA1220) ; 41304073) ; 41304073)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/86410]
专题	中国科学院地质与地球物理研究所
通讯作者	Ren, Zhikun
作者单位	1.China Earthquake Adm, Inst Geol, State Key Lab Earthquake Dynam, Beijing 100029, Peoples R China 2.Kyoto Univ, Grad Sch Sci, Dept Geophys, Kyoto 6068502, Japan 3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Ren, Zhikun,Zhang, Zhuqi,Dai, Fuchu,et al. Topographic changes due to the 2008 Mw 7.9 Wenchuan earthquake as revealed by the differential DEM method[J]. GEOMORPHOLOGY,2014,217:122-130.
APA	Ren, Zhikun,Zhang, Zhuqi,Dai, Fuchu,Yin, Jinhui,&Zhang, Huiping.(2014).Topographic changes due to the 2008 Mw 7.9 Wenchuan earthquake as revealed by the differential DEM method.GEOMORPHOLOGY,217,122-130.
MLA	Ren, Zhikun,et al."Topographic changes due to the 2008 Mw 7.9 Wenchuan earthquake as revealed by the differential DEM method".GEOMORPHOLOGY 217(2014):122-130.