Precisiones estratigráficas sobre el límite inferior de la Formación Artés (Paleógeno, cuenca del Ebro)

dc.contributor.authorLópez Blanco, Miguel
dc.contributor.authorPiña, J.
dc.contributor.authorMarzo, M.
dc.date.accessioned2017-07-31T11:21:34Z
dc.date.available2017-07-31T11:21:34Z
dc.date.issued1994
dc.description.abstractAccording to its original definition, the Artes Formation is formed by the ensemble of continental, red mudstones and sandstones interbedded with conglomerates resting on top of the marine deposits of the Bartonian to Priabonian Santa Maria Croup. However, detailed mapping clearly shows that those marine rocks are laterally equivalent to distal alluvial fan facies of the "Artes type". On the basis of our present sedimentological knowledge these facies can not be differentiated from those forming the Artes Formation sensu stricto .Therefore, we propose a new definition for the entire formation that includes its subdivision into two memberses_ES
dc.identifier.urihttp://hdl.handle.net/10272/14007
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherLithostratigraphyes_ES
dc.subject.otherDistal alluvial fan facies,es_ES
dc.subject.otherEbro basines_ES
dc.titlePrecisiones estratigráficas sobre el límite inferior de la Formación Artés (Paleógeno, cuenca del Ebro)es_ES
dc.titleOn the lower boundary of the Artés Formation (Paleogene, Ebro basin)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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