Barcelona, España
Bari, Italia
Jaén, España
This study is a first attempt to reproduce seismites in laboratory using a shaking table and natural sediments. The deformation linked to liquefaction-fluidization processes has been analysed, continously 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 column.
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