Estructuras sedimentarias de deformación (sismitas) inducidas por licuefacción con un simulador de terremotos
This 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 stru...
| Autores: | , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1996 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/11084 |
| Acceso en línea: | http://hdl.handle.net/10272/11084 |
| Access Level: | acceso abierto |
| Palabra clave: | Liquefaction Selsmites Shaking table Soft-sediment deformation structures |
| Sumario: | This 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 column |
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