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<dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:invenio="http://invenio-software.org/elements/1.0" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><dc:identifier>doi:10.1016/j.marpetgeo.2018.05.032</dc:identifier><dc:language>eng</dc:language><dc:creator>Val, J.</dc:creator><dc:creator>Bádenas, B.</dc:creator><dc:creator>Aurell, M.</dc:creator><dc:title>Sedimentary architecture of a prograding oolitic-siliciclastic wedge: Response to changes in wave-base oscillation (Kimmeridgian, Iberian Basin)</dc:title><dc:identifier>ART-2018-107053</dc:identifier><dc:description>A detailed facies and sequential architectural analysis has been carried out along the wedge-shaped shallow marine cross-bedded oolitic-siliciclastic Ricla Member (Kimmeridgian, Northern Iberian Basin). The obtained results are based on fieldwork along the 4 × 1 km continuous outcrops with the use of high-resolution photomosaics and drone-made videos, which have led to a precise and extensive facies reconstruction. Three main facies that are laterally related (A to B to C) in down-dip direction have been differentiated, which correspond to the topset, foreset and bottomset parts of a sloping depositional surface. Sedimentation was controlled by sweeping drift and downwelling storm-induced currents causing avalanching processes, with the deep action of oscillatory currents. The sedimentary architecture consists in 5 successive units composed by several sub-units, arranged according to different stacking patterns, which reflect the sedimentary response to wave-base oscillations superimposed to the regressive part of a third-order transgressive-regressive cycle. The sedimentological features indicate that this unit, which has been previously interpreted as a dune complex fit with an infralittoral prograding wedge model, as it is observed in geographically close and stratigraphically similar units. The Ricla Member is therefore regarded as an example of a well-exposed grain-supported unit with broad potential application to other prograding grain-dominated lithosomes that do not conform to the traditional sand shoal model.</dc:description><dc:date>2018</dc:date><dc:source>http://zaguan.unizar.es/record/79356</dc:source><dc:doi>10.1016/j.marpetgeo.2018.05.032</dc:doi><dc:identifier>http://zaguan.unizar.es/record/79356</dc:identifier><dc:identifier>oai:zaguan.unizar.es:79356</dc:identifier><dc:relation>info:eu-repo/grantAgreement/ES/DGA/H54-Grupos Consolidados</dc:relation><dc:relation>info:eu-repo/grantAgreement/ES/MINECO-FEDER/CGL2017-85038-P</dc:relation><dc:identifier.citation>MARINE AND PETROLEUM GEOLOGY 96 (2018), 113-127</dc:identifier.citation><dc:rights>by-nc-nd</dc:rights><dc:rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights><dc:rights>info:eu-repo/semantics/openAccess</dc:rights></dc:dc>

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