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• W2020389634 abstract "Recent studies have pointed out a similarity between tectonics and slope tectonic-induced structures. Numerous studies have demonstrated that structures and fabrics previously interpreted as of purely geodynamical origin are instead the result of large slope deformation, and this led in the past to erroneous interpretations. Nevertheless, their limit seems not clearly defined, but it is somehow transitional. Some studies point out continuity between failures developing at surface with upper crust movements. In this contribution, the main studies which examine the link between rock structures and slope movements are reviewed. The aspects regarding model and scale of observation are discussed together with the role of pre-existing weaknesses in the rock mass. As slope failures can develop through progressive failure, structures and their changes in time and space can be recognized. Furthermore, recognition of the origin of these structures can help in avoiding misinterpretations of regional geology. This also suggests the importance of integrating different slope movement classifications based on distribution and pattern of deformation and the application of structural geology techniques. A structural geology approach in the landslide community is a tool that can greatly support the hazard quantification and related risks, because most of the physical parameters, which are used for landslide modeling, are derived from geotechnical tests or the emerging geophysical approaches." @default.
• W2020389634 created "2016-06-24" @default.
• W2020389634 creator A5031270872 @default.
• W2020389634 creator A5035046919 @default.
• W2020389634 creator A5047247987 @default.
• W2020389634 creator A5058942509 @default.
• W2020389634 creator A5079139797 @default.
• W2020389634 date "2013-10-01" @default.
• W2020389634 modified "2023-09-25" @default.
• W2020389634 title "An introductory review on gravitational-deformation induced structures, fabrics and modeling" @default.
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