Estructuras de deformación en sedimentos del Cuaternario reciente de la cuenca del Bajo Segura. (Alicante). Discusión sobre su posible origen sísmico

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dc.contributor.authorAlfaro García, Pedro
dc.contributor.authorDoménech, C.
dc.contributor.authorEstévez, Antonio
dc.contributor.authorSoria, Jesús M.
dc.date.accessioned2017-06-13T12:14:19Z
dc.date.available2017-06-13T12:14:19Z
dc.date.issued1994
dc.description.abstractAiming at recognizing the prints in the most recent sedimentary record due to earthquakes, able to develop liquefaction and fluidization in sediments (magnitude equal to or more than 5), we have studied eight boreholes, each about 40 m long, located in the Low Segura basin (Alicante, Spain). We have recognized disturbances due to the own boring activity, as well as others due to bioturbation, thixotropy in clayey levels and to what, in our opinion, is the effect of seismic shocks (microfaults, distorted lamination and fluid scape structures)en_US
dc.identifier.urihttp://hdl.handle.net/10272/13839
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.otherPaleoseismicityen_US
dc.subject.otherSeismitesen_US
dc.subject.otherActive tectonicsen_US
dc.subject.otherQuaternaryen_US
dc.subject.otherBetic Cordilleraen_US
dc.subject.otherAlicanteen_US
dc.titleEstructuras de deformación en sedimentos del Cuaternario reciente de la cuenca del Bajo Segura. (Alicante). Discusión sobre su posible origen sísmicoen_US
dc.titleDeformation structures in late Quaternary sediments from the Low Segura basin (Alicante). A discussion about their seismic origineng
dc.typeconference outputen_US
dspace.entity.typePublication

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Geogaceta -- Nº 17, (1994)