Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/96472
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dc.contributorMainland Development Office-
dc.creatorZhang, Hen_US
dc.creatorWu, Yen_US
dc.creatorHuang, Sen_US
dc.creatorZheng, Len_US
dc.creatorMiao, Yen_US
dc.date.accessioned2022-12-07T02:55:04Z-
dc.date.available2022-12-07T02:55:04Z-
dc.identifier.urihttp://hdl.handle.net/10397/96472-
dc.language.isoenen_US
dc.publisherFrontiers Research Foundationen_US
dc.rights© 2022 Zhang, Wu, Huang, Zheng and Miao. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY) (https://creativecommons.org/licenses/by/4.0/). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.en_US
dc.rightsThe following publication Zhang, H., Wu, Y., Huang, S., Zheng, L., & Miao, Y. (2022). Analysis of flexural toppling failure of anti-dip rock slopes due to earthquakes. Frontiers in Earth Science, 9, 831023 is available at https://doi.org/10.3389/feart.2021.831023.en_US
dc.subjectAnti-dip rock slopeen_US
dc.subjectFlexural topplingen_US
dc.subjectLimit equilibriumen_US
dc.subjectSeismic loaden_US
dc.subjectStability analysisen_US
dc.titleAnalysis of flexural toppling failure of anti-dip rock slopes due to earthquakesen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume9en_US
dc.identifier.doi10.3389/feart.2021.831023en_US
dcterms.abstractFlexural toppling is one of the failure modes of anti-dip rocks, is often triggered by seismic load, occurs haphazardly under an earthquake scenario, and is characterized by high speed and extreme energy, leading to catastrophic disaster consequences and huge losses. However, there is limited literature that reveals its failure mechanisms and describes the failure surface due to earthquakes. Therefore, based on the limit equilibrium analysis method, the horizontal pseudo-static load was applied to improve the geological mechanical model under gravity only, and the stability analysis process was derived. The failure surface and failure mode of the slope under different seismic loads were analyzed. The results indicated that, with the increasing seismic load, an increase in the number of rock layers with sliding failure increased the number of rock layers with cantilever toppling failure; in contrast, the number of rock layers with overlapping toppling failure decreased. The slope toe was more prone to sliding and the slope top was more prone to cantilever toppling under an earthquake, which decreased the stability of the anti-dip rock slope.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationFrontiers in earth science, Jan. 2022, v. 9, 831023en_US
dcterms.isPartOfFrontiers in earth scienceen_US
dcterms.issued2022-01-
dc.identifier.scopus2-s2.0-85124527729-
dc.identifier.eissn2296-6463en_US
dc.identifier.artn831023en_US
dc.description.validate202212 bckw-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOS-
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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