Estructuras sedimentarias de deformación (sismitas) inducidas por licuefacción con un simulador de terremotos

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dc.contributor.authorCaselles, J. O.
dc.contributor.authorMoretti, M.
dc.contributor.authorAlfaro García, Pedro
dc.contributor.authorCanas, J. A.
dc.contributor.authorClapés, J.
dc.date.accessioned2015-09-02T09:33:33Z
dc.date.available2015-09-02T09:33:33Z
dc.date.issued1996
dc.description.abstractThis study is a first attempt to reproduce se¡smites in laboratory using a shaking table and natural sediments. The deformation linked to liquefaction-fluidization processes has been analysed, contlnously controlling the Interstitial pressure and acceleration. Morphologically, two main types of structures have been observed: fluid escape and load. The morphological variety is primarily controlled by the type of sedimentary columnen_US
dc.identifier.urihttp://hdl.handle.net/10272/11084
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherLiquefactionen_US
dc.subject.otherSelsmitesen_US
dc.subject.otherShaking tableen_US
dc.subject.otherSoft-sediment deformation structuresen_US
dc.titleEstructuras sedimentarias de deformación (sismitas) inducidas por licuefacción con un simulador de terremotosen_US
dc.titleSoft-sediment deformation structures (seismites) induced by liquefaction with a digital shaking tableeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 21 (1996)