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Stratigraphy of the Santa Orosia fan delta (middle and upper Eocene, Jaca Basin Huesca prov. Spain)

dc.contributor.authorOms, O.
dc.contributor.authorRemacha Grau, Eduard
dc.date.accessioned2019-06-03T11:08:34Z
dc.date.available2019-06-03T11:08:34Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/10272/16336
dc.description.abstractThe study of the Santa Orosia fan delta north of the Basa anticline (Jaca Basin, Southern Pyrenees) has described the type 2 Jaca-6 sequence. The upper Sabihinigo sandstone, storm and tidal influenced, enhaces the shelf margin systems tract, being conformable to the West and unconformable to the East due to a tectonic relief developed by the Bini4s thrust. The transgressive systems tract is the conformable lowermost part of the Pamplona offshore marls that are onlapping to the east the lo w er and m iddle Sabifidnigo Sandstone. The highstand systems tract are the rest o f the offshore Pamplona marls gradding to mouth bars sandstones and this to alluvial conglomerate deposits capped by the erosional surface of the Jaca complex unconformity topes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherPyreneeses_ES
dc.subject.otherEocenees_ES
dc.subject.otherJaca basines_ES
dc.subject.otherSequence-stratigraphyes_ES
dc.subject.otherFan deltaes_ES
dc.titleEstratigrafía del abanico deltaico de Santa Orosia (Eoceno medio y superior de la cuenca de Jaca, Prov. de Huesca)es_ES
dc.titleStratigraphy of the Santa Orosia fan delta (middle and upper Eocene, Jaca Basin Huesca prov. Spain)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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