Caselles, J. O.Moretti, M.Alfaro García, PedroCanas, J. A.Clapés, J.2015-09-022015-09-021996http://hdl.handle.net/10272/11084This 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 columnspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/LiquefactionSelsmitesShaking tableSoft-sediment deformation structuresjournal articleopen access