1. Studi Geologici Camerti
  2. 2 - Studi Geologici Camerti - Volume Speciale
  3. 2002: International workshop "Large-scale vertical movements and related gravitational processes", Camerino-Roma 21th-26th June, 1999, Proceedings
Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1357
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Campo DCValoreLingua
dc.contributor.authorCANDIO, S.-
dc.contributor.authorCATTUTO, C.-
dc.contributor.authorGREGORI, L.-
dc.contributor.authorMELELLI, L.-
dc.contributor.authorTARAMELLI, A.-
dc.date.accessioned2017-12-06T13:54:10Z-
dc.date.available2017-12-06T13:54:10Z-
dc.date.issued2002-
dc.identifier.citationStudi geologici camerti, n. speciale, 2002, pp. 29-36it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/732-
dc.description.abstractTwo examples of deep-seated gravitational slope deforma­tions involving materials of complex behaviour (sensu CARRARA et al., 1987) are studied in this work. Rocks with complex behaviour are generally terrigenous rocks with sandy and marly alternation (generally flysch deposits). The evolution of these examples was caused fundamentally by movements of tectonic uplift which have occurred in the centra! areas of .the ltalian peninsular with a maxi­mum in the lower Pleistocene. [...]en
dc.publisherUniversità di Camerinoit
dc.subjectCentral Apennine - Deep-seated Gravitational Slope Deformation (D.G.S.D.) - Landslide - Uplift - Terrigenous - Tectonicen
dc.subjectAppennino centrale - Deformazione Gravitativa Profonda di Versante (D.G.P.V.) - Frana - Sollevamento - Terrigeno - Tettonicait
dc.titleSOME EXAMPLES OF DEEP-SEATED GRAVITATATIONAL SLOPE DEFORMATION AND LARGE-SCALE LANDSLIDES CAUSED BY TECTONIC UPLIFT IN TERRIGENOUS MATERIALS IN UMBRIA AND BOUNDERING AREASen
dc.description.pages29-36-
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