Influencia diapírica sobre depósitos fluviales de tipo «braided» en la cantera de Laño (Campaniense Superior-Maastrichtiense Inferior. Cuenca Vasco-Cantábrica)

dc.contributor.authorGómez Alday, Juan José
dc.contributor.authorElorza, Javier
dc.date.accessioned2015-03-26T13:09:06Z
dc.date.available2015-03-26T13:09:06Z
dc.date.issued1998
dc.description.abstractThe western cliff of the Laño quarry shows extensive tabular sandsheet bodies of upper Campanian-lower Maastrichtian age, that represent channel-fill sequences deposited in a broad low-sinuosity braided-type fluvial system. Diverse sedimentological features such as channel incision, bedform types and palaeocurrent distribution, as well as the occurrence of seism related structures are interpreted in terms of possible synsedimentary tectonic activity of the very close Peñacerrada Diapiren_US
dc.identifier.urihttp://hdl.handle.net/10272/10178
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.otherCampanian-Maastrichtianen_US
dc.subject.otherBraided-type fluvial depositsen_US
dc.subject.otherSynsedimentary tectonic activityen_US
dc.subject.otherPeñacerrada Diapiren_US
dc.titleInfluencia diapírica sobre depósitos fluviales de tipo «braided» en la cantera de Laño (Campaniense Superior-Maastrichtiense Inferior. Cuenca Vasco-Cantábrica)en_US
dc.titleDiapiric influence upon braided-type fluvial deposits at the Laño quarry (Upper Campanian-Lower Maastrichtian. Basque-Cantabrian Basin)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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