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Paleoseismicity related to the Devonian-Carboniferous boundary in the South-Portuguese Zone (SW Iberia)

dc.contributor.authorMoreno Garrido, María Carmen 
dc.contributor.authorSáez Ramos, Reinaldo 
dc.contributor.authorGonzález Barrionuevo, Felipe 
dc.date.accessioned2014-06-26T12:34:39Z
dc.date.available2014-06-26T12:34:39Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/10272/8374
dc.description.abstractIn this paper several evidences of seismic activity in the latest Devonian deposits of the South Portuguese Zone are reported. They are represented by deposits and sedimentary structures associated with processes such sediment liquefactions and fluidifications, tsunamis, fracturations, synsedimentary deformations, slidings or mass flows, that were generated during the rupture and shaking of the ground. As a result, two different levels of seismites related with two major paleoseismic events have been identified in SW Iberian close to the D-C boundaryen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherPaleoseismicityen_US
dc.subject.otherDevonian-Carboniferous boundaryen_US
dc.subject.otherSouth Portuguese Zoneen_US
dc.titlePaleosismicidad asociada al tránsito Devónico – Carbonífero en la Zona Surportuguesa (SW Ibérico)en_US
dc.titlePaleoseismicity related to the Devonian-Carboniferous boundary in the South-Portuguese Zone (SW Iberia)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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