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Upper Albian Transgressive marine deposits in the terrigenous series of the "Páramo de la Lora" (northern side, Cantabria and Palencia, Spain)

dc.contributor.authorMartínez de Rituerto Ibisate, S.
dc.contributor.authorGarcía Mondéjar, Joaquín
dc.date.accessioned2014-12-12T10:55:10Z
dc.date.available2014-12-12T10:55:10Z
dc.date.issued2001
dc.identifier.urihttp://hdl.handle.net/10272/9523
dc.description.abstractThe Lower Cretaceous series of the northern side of the "Páramo de la Lora" is mainly continental fluvial. A detailed analysis of the section outcropping between Cuillas del Valle and Olleros de Paredes Rubias, has revealed fades which can be attributed to transitional continental-marine enviroments. These are horizontally bedded sandstones with oscillation ripples (lagoon and shoreface), and cross-stratified sandstones with backset laminae (tidal). Other cross-stratified sandstones (fluvial channels), laminated lutites (alluvial coastal plain), bivalve sandstones (tidal ?) and lutites with leaves (marsh), make up contemporaneously-related subenvironments. Storm wave action prevailed during the filling of a narrow erosional depression, and tidal action accompanied the later establishment of valleywide sedimentary conditionsen_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.otherLittoralen_US
dc.subject.otherTidal faciesen_US
dc.subject.otherValley fillen_US
dc.subject.otherUpper Albianen_US
dc.subject.otherOllerosen_US
dc.subject.otherLa Loraen_US
dc.titleDepósitos de transgresión marina del Albiense superior en la serie terrígena del Páramo de la Lora (vertiente norte, Cantabria y Palencia)en_US
dc.titleUpper Albian Transgressive marine deposits in the terrigenous series of the "Páramo de la Lora" (northern side, Cantabria and Palencia, Spain)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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