Dynamic response of the Daguangbao landslide triggered by the Wenchuan earthquake with a composite hypocenter

To identify the correspondence between the different dynamic responses of the Daguangbao landslide and the different faulting mechanisms of the composite-hypocenter, the whole hypocenter of the Wenchuan earthquake was divided into four sub-hypocenters. On another hand, based on the location of the D...

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Main Authors: Fangpeng Cui, Chen Xiong, Qiang Wu, Chong Xu, Ning Li, Ning'an Wu, Li Cui
Format: Article
Language:English
Published: Taylor & Francis Group 2021-01-01
Series:Geomatics, Natural Hazards & Risk
Subjects:
Online Access:http://dx.doi.org/10.1080/19475705.2021.1944916
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author Fangpeng Cui
Chen Xiong
Qiang Wu
Chong Xu
Ning Li
Ning'an Wu
Li Cui
author_facet Fangpeng Cui
Chen Xiong
Qiang Wu
Chong Xu
Ning Li
Ning'an Wu
Li Cui
author_sort Fangpeng Cui
collection DOAJ
description To identify the correspondence between the different dynamic responses of the Daguangbao landslide and the different faulting mechanisms of the composite-hypocenter, the whole hypocenter of the Wenchuan earthquake was divided into four sub-hypocenters. On another hand, based on the location of the Dauangbao landslide, the composite-hypocenter was divided into the Initial Sub-hypocenter, the Approaching Sub-hypocenter, the Local Sub-hypocenter, the Receding sub-hypocenter and the Terminal sub-hypocenter. Subsequently, dynamic response of the landslide was modeled by using UDEC software. The results show that progressive damage and critical failure of the mega landslide are triggered by the second sub-hypocenter. Simutaneously, with respect to the second classification basis, its progressive damage is induced by the Approaching Hypocenter and the Local Hypocenter in time sequence. The Local Hypocenter triggers its critical failure. During the long-runout stage, besides the local topography, its self-gravity poses a dominant contribution to the dynamic responses of the landslide. Especially, the inertial seismic force is another key factor that triggers the ejection stage of the landslide. The following seismic forces triggered by the corresponding sub-hypocenter influence the long-runout stage slightly. The horizontal seismic force poses a dominant contribution to the progressive damage and critical failure of the mega landslide.
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spelling doaj.art-8fc1b1771d3f4ad0834a622146e92b0d2022-12-21T23:48:26ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132021-01-011212170219310.1080/19475705.2021.19449161944916Dynamic response of the Daguangbao landslide triggered by the Wenchuan earthquake with a composite hypocenterFangpeng Cui0Chen Xiong1Qiang Wu2Chong Xu3Ning Li4Ning'an Wu5Li Cui6School of Geoscience and Surveying Engineering, China University of Mining and Technology-BeijingSchool of Geoscience and Surveying Engineering, China University of Mining and Technology-BeijingSchool of Geoscience and Surveying Engineering, China University of Mining and Technology-BeijingInstitute of Geology, China Earthquake Administration, Beijing ChinaSchool of Geoscience and Surveying Engineering, China University of Mining and Technology-BeijingSchool of Geoscience and Surveying Engineering, China University of Mining and Technology-BeijingSchool of Geoscience and Surveying Engineering, China University of Mining and Technology-BeijingTo identify the correspondence between the different dynamic responses of the Daguangbao landslide and the different faulting mechanisms of the composite-hypocenter, the whole hypocenter of the Wenchuan earthquake was divided into four sub-hypocenters. On another hand, based on the location of the Dauangbao landslide, the composite-hypocenter was divided into the Initial Sub-hypocenter, the Approaching Sub-hypocenter, the Local Sub-hypocenter, the Receding sub-hypocenter and the Terminal sub-hypocenter. Subsequently, dynamic response of the landslide was modeled by using UDEC software. The results show that progressive damage and critical failure of the mega landslide are triggered by the second sub-hypocenter. Simutaneously, with respect to the second classification basis, its progressive damage is induced by the Approaching Hypocenter and the Local Hypocenter in time sequence. The Local Hypocenter triggers its critical failure. During the long-runout stage, besides the local topography, its self-gravity poses a dominant contribution to the dynamic responses of the landslide. Especially, the inertial seismic force is another key factor that triggers the ejection stage of the landslide. The following seismic forces triggered by the corresponding sub-hypocenter influence the long-runout stage slightly. The horizontal seismic force poses a dominant contribution to the progressive damage and critical failure of the mega landslide.http://dx.doi.org/10.1080/19475705.2021.1944916a composite hypocentredip-slip faulting mechanismoblique-slip faulting mechanismstrike-slip faulting mechanisminitial sub-hypocenterlocal sub-hypocenterterminal sub-hypocenter
spellingShingle Fangpeng Cui
Chen Xiong
Qiang Wu
Chong Xu
Ning Li
Ning'an Wu
Li Cui
Dynamic response of the Daguangbao landslide triggered by the Wenchuan earthquake with a composite hypocenter
Geomatics, Natural Hazards & Risk
a composite hypocentre
dip-slip faulting mechanism
oblique-slip faulting mechanism
strike-slip faulting mechanism
initial sub-hypocenter
local sub-hypocenter
terminal sub-hypocenter
title Dynamic response of the Daguangbao landslide triggered by the Wenchuan earthquake with a composite hypocenter
title_full Dynamic response of the Daguangbao landslide triggered by the Wenchuan earthquake with a composite hypocenter
title_fullStr Dynamic response of the Daguangbao landslide triggered by the Wenchuan earthquake with a composite hypocenter
title_full_unstemmed Dynamic response of the Daguangbao landslide triggered by the Wenchuan earthquake with a composite hypocenter
title_short Dynamic response of the Daguangbao landslide triggered by the Wenchuan earthquake with a composite hypocenter
title_sort dynamic response of the daguangbao landslide triggered by the wenchuan earthquake with a composite hypocenter
topic a composite hypocentre
dip-slip faulting mechanism
oblique-slip faulting mechanism
strike-slip faulting mechanism
initial sub-hypocenter
local sub-hypocenter
terminal sub-hypocenter
url http://dx.doi.org/10.1080/19475705.2021.1944916
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