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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:10.1007/s10347-018-0521-8</dc:identifier><dc:language>eng</dc:language><dc:creator>Sequero, C.</dc:creator><dc:creator>Bádenas, B.</dc:creator><dc:creator>Aurell, M.</dc:creator><dc:title>Facies mosaic in the inner areas of a shallow carbonate ramp (Upper Jurassic, Higueruelas Fm, NE Spain)</dc:title><dc:identifier>ART-2018-104550</dc:identifier><dc:description>The internal facies and sedimentary architecture of an Upper Jurassic inner carbonate ramp were reconstructed after the analysis and correlation of 14 logs in a 1 × 2 km outcrop area around the Mezalocha locality (south of Zaragoza, NE Spain). The studied interval is 10–16 m thick and belongs to the upper part of the uppermost Kimmeridgian–lower Tithonian Higueruelas Fm. On the basis of texture and relative proportion of the main skeletal and non-skeletal components, 6 facies and 12 subfacies were differentiated, which record subtidal (backshoal/washover, sheltered lagoon and pond/restricted lagoon) to intertidal subenvironments. The backshoal/washover subenvironment is characterized by peloidal wackestone–packstone and grainstone. The lagoon subenvironment includes oncolitic, stromatoporoid, and oncolitic-stromatoporoid (wackestone and packstone) facies. The intertidal subenvironment is represented by peloidal mudstone and packstone–grainstone with fenestral porosity. Gastropod-oncolitic (wackestone–packstone and grainstone) facies with intercalated marl may reflect local ponds in the intertidal or restricted lagoon subenvironments. Detailed facies mapping allowed us to document 7 sedimentary units within a general shallowing-upward trend, which reflect a mosaic distribution, especially for stromatoporoid and fenestral facies, with facies patches locally more than 500 m in lateral extent. External and internal factors controlled this heterogeneity, including resedimentation, topographic relief and substrate stability, combined with variations in sea-level. This mosaic facies distribution provides useful tools for more precise reconstructions of depositional heterogeneities, and this variability must be taken into account in order to obtain a solid sedimentary framework at the kilometer scale..</dc:description><dc:date>2018</dc:date><dc:source>http://zaguan.unizar.es/record/77068</dc:source><dc:doi>10.1007/s10347-018-0521-8</dc:doi><dc:identifier>http://zaguan.unizar.es/record/77068</dc:identifier><dc:identifier>oai:zaguan.unizar.es:77068</dc:identifier><dc:relation>info:eu-repo/grantAgreement/ES/MINECO/CGL2014-53548-P</dc:relation><dc:relation>info:eu-repo/grantAgreement/ES/MINECO/CGL2017-85038-P</dc:relation><dc:relation>info:eu-repo/grantAgreement/ES/UZ/IUCA-H54</dc:relation><dc:identifier.citation>FACIES 64, 2 (2018), 9 [23 pp]</dc:identifier.citation><dc:rights>All rights reserved</dc:rights><dc:rights>http://www.europeana.eu/rights/rr-f/</dc:rights><dc:rights>info:eu-repo/semantics/openAccess</dc:rights></dc:dc>

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