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Paleoseismic structures in hidromagmatic deposits of the Neogene volcanism in the Campo de Calatrava, Ciudad Real (Spain)

dc.contributor.authorRodríguez Pascua, M. A.
dc.contributor.authorBarrera Morate, J. L.
dc.date.accessioned2014-11-17T12:49:15Z
dc.date.available2014-11-17T12:49:15Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9317
dc.description.abstractPaleoseismic structures are described for the first time in the volcanism of Campo de Calatrava. The structures are located in hydromagmatic deposits of maars. This study allows to detect seismic activity after the last Quaternary eruptions in the Granatura - Moral Basin (Neogene Age). The liquefied sediments are conglomerates (lapilli) and the seismic magnitude to liquely this coarse-grained sediment should be higher than 7.5.en_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSeismitesen_US
dc.subject.otherPyroclastic depositsen_US
dc.subject.otherVolcanismen_US
dc.subject.otherCranátulaen_US
dc.titleEstructuras paleosísmicas en depósitos h¡dromagmáticos del vulcanismo neógeno del Campo de Calatrava, Ciudad Real (España)en_US
dc.titlePaleoseismic structures in hidromagmatic deposits of the Neogene volcanism in the Campo de Calatrava, Ciudad Real (Spain)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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