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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:language>eng</dc:language><dc:creator>Ibáñez, A.</dc:creator><dc:creator>Soria De Miguel, Ana Rosa</dc:creator><dc:creator>Liesa Carrera, Carlos Luis</dc:creator><dc:title>Sedimentology and sedimentary evolution of the Artoles Fm in Miravete de la Sierra (Teruel, Iberian Chain)</dc:title><dc:identifier>ART-2015-95866</dc:identifier><dc:description>The sedimentology and sedimentary evolution of the Barremian Artoles Fm in the Camino de Miravete section (Galve sub-basin, Spain) is presented. The detailed log of the stratigraphic succession together with facies analysis and fossil content have allowed the distinction of four main facies associations: mixed terrigenous-carbonate lagoon, flood-tidal delta, proximal middle ramp and distal middle ramp. The sedimentary evolution of facies associations characterizes three successive stages: I- restricted carbonate lagoon system, II- middle ramp system and III- turning back to another carbonate lagoon with more open facies. Eustasy and tectonics may be responsible of the abrupt deepening that took place between stages I and II.</dc:description><dc:date>2015</dc:date><dc:source>http://zaguan.unizar.es/record/56655</dc:source><dc:identifier>http://zaguan.unizar.es/record/56655</dc:identifier><dc:identifier>oai:zaguan.unizar.es:56655</dc:identifier><dc:relation>info:eu-repo/grantAgreement/ES/MICINN/CGL2011-23717</dc:relation><dc:identifier.citation>Geogaceta 58 (2015), 11-14</dc:identifier.citation><dc:rights>by-nc</dc:rights><dc:rights>http://creativecommons.org/licenses/by-nc/3.0/es/</dc:rights><dc:rights>info:eu-repo/semantics/openAccess</dc:rights></dc:dc>

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