El surco de Aia-Zaldibia (Aptiense inferior, Aralar, Gipuzkoa)

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dc.contributor.authorLertxundi, D.
dc.contributor.authorGarcía Mondéjar, Joaquín
dc.date.accessioned2015-05-11T09:40:11Z
dc.date.available2015-05-11T09:40:11Z
dc.date.issued1997
dc.description.abstractDetailed mapping, facies analysis and thickness distribution of a lower Aptian succession in the Aralar area, led to the establishment of a sedimentary trough for the early Aptian in the Aia-Zaldibia section. The trough was located on a carbonate platform and was filled with high energy mixed terrigenous and carbonate materials attributed to an estuarine environment. N-S oriented synsedimentary deep tectonic control is Invoked to explaint he trough origin and its developmenten_US
dc.identifier.urihttp://hdl.handle.net/10272/10545
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.otherSedimentary troughen_US
dc.subject.otherTidal channelen_US
dc.subject.otherTectonic controlen_US
dc.subject.otherLower Aptianen_US
dc.subject.otherAia-Zaldibiaen_US
dc.subject.otherAralaren_US
dc.titleEl surco de Aia-Zaldibia (Aptiense inferior, Aralar, Gipuzkoa)en_US
dc.titleThe Aia-Zaldibia trough (Lower Aptian, Aralar, Gipuzkoa)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 22, (1997)