<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
    <record>
        <controlfield tag="001">79356</controlfield>
        <controlfield tag="005">20200117221630.0</controlfield>
        <datafield tag="024" ind1="7" ind2=" ">
            <subfield code="2">doi</subfield>
            <subfield code="a">10.1016/j.marpetgeo.2018.05.032</subfield>
        </datafield>
        <datafield tag="024" ind1="8" ind2=" ">
            <subfield code="2">sideral</subfield>
            <subfield code="a">107053</subfield>
        </datafield>
        <datafield tag="037" ind1=" " ind2=" ">
            <subfield code="a">ART-2018-107053</subfield>
        </datafield>
        <datafield tag="041" ind1=" " ind2=" ">
            <subfield code="a">eng</subfield>
        </datafield>
        <datafield tag="100" ind1=" " ind2=" ">
            <subfield code="0">(orcid)0000-0001-8777-6984</subfield>
            <subfield code="a">Val, J.</subfield>
        </datafield>
        <datafield tag="245" ind1=" " ind2=" ">
            <subfield code="a">Sedimentary architecture of a prograding oolitic-siliciclastic wedge: Response to changes in wave-base oscillation (Kimmeridgian, Iberian Basin)</subfield>
        </datafield>
        <datafield tag="260" ind1=" " ind2=" ">
            <subfield code="c">2018</subfield>
        </datafield>
        <datafield tag="506" ind1="0" ind2=" ">
            <subfield code="a">Access copy available to the general public</subfield>
            <subfield code="f">Unrestricted</subfield>
        </datafield>
        <datafield tag="520" ind1="3" ind2=" ">
            <subfield code="a">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.</subfield>
        </datafield>
        <datafield tag="536" ind1=" " ind2=" ">
            <subfield code="9">info:eu-repo/grantAgreement/ES/DGA/H54-Grupos Consolidados</subfield>
            <subfield code="9">info:eu-repo/grantAgreement/ES/MINECO-FEDER/CGL2017-85038-P</subfield>
        </datafield>
        <datafield tag="540" ind1=" " ind2=" ">
            <subfield code="9">info:eu-repo/semantics/openAccess</subfield>
            <subfield code="a">by-nc-nd</subfield>
            <subfield code="u">http://creativecommons.org/licenses/by-nc-nd/3.0/es/</subfield>
        </datafield>
        <datafield tag="590" ind1=" " ind2=" ">
            <subfield code="a">3.538</subfield>
            <subfield code="b">2018</subfield>
        </datafield>
        <datafield tag="591" ind1=" " ind2=" ">
            <subfield code="a">GEOSCIENCES, MULTIDISCIPLINARY</subfield>
            <subfield code="b">39 / 195 = 0.2</subfield>
            <subfield code="c">2018</subfield>
            <subfield code="d">Q1</subfield>
            <subfield code="e">T1</subfield>
        </datafield>
        <datafield tag="592" ind1=" " ind2=" ">
            <subfield code="a">1.459</subfield>
            <subfield code="b">2018</subfield>
        </datafield>
        <datafield tag="593" ind1=" " ind2=" ">
            <subfield code="a">Economic Geology</subfield>
            <subfield code="c">2018</subfield>
            <subfield code="d">Q1</subfield>
        </datafield>
        <datafield tag="593" ind1=" " ind2=" ">
            <subfield code="a">Geology</subfield>
            <subfield code="c">2018</subfield>
            <subfield code="d">Q1</subfield>
        </datafield>
        <datafield tag="593" ind1=" " ind2=" ">
            <subfield code="a">Stratigraphy</subfield>
            <subfield code="c">2018</subfield>
            <subfield code="d">Q1</subfield>
        </datafield>
        <datafield tag="593" ind1=" " ind2=" ">
            <subfield code="a">Oceanography</subfield>
            <subfield code="c">2018</subfield>
            <subfield code="d">Q1</subfield>
        </datafield>
        <datafield tag="593" ind1=" " ind2=" ">
            <subfield code="a">Geophysics</subfield>
            <subfield code="c">2018</subfield>
            <subfield code="d">Q1</subfield>
        </datafield>
        <datafield tag="655" ind1=" " ind2="4">
            <subfield code="a">info:eu-repo/semantics/article</subfield>
            <subfield code="v">info:eu-repo/semantics/acceptedVersion</subfield>
        </datafield>
        <datafield tag="700" ind1=" " ind2=" ">
            <subfield code="0">(orcid)0000-0003-1112-524X</subfield>
            <subfield code="a">Bádenas, B.</subfield>
            <subfield code="u">Universidad de Zaragoza</subfield>
        </datafield>
        <datafield tag="700" ind1=" " ind2=" ">
            <subfield code="0">(orcid)0000-0002-2430-7424</subfield>
            <subfield code="a">Aurell, M.</subfield>
            <subfield code="u">Universidad de Zaragoza</subfield>
        </datafield>
        <datafield tag="710" ind1="2" ind2=" ">
            <subfield code="1">2000</subfield>
            <subfield code="2">280</subfield>
            <subfield code="a">Universidad de Zaragoza</subfield>
            <subfield code="b">Dpto. Ciencias de la Tierra</subfield>
            <subfield code="c">Área Estratigrafía</subfield>
        </datafield>
        <datafield tag="773" ind1=" " ind2=" ">
            <subfield code="g">96 (2018), 113-127</subfield>
            <subfield code="p">Mar. pet. geol.</subfield>
            <subfield code="t">MARINE AND PETROLEUM GEOLOGY</subfield>
            <subfield code="x">0264-8172</subfield>
        </datafield>
        <datafield tag="856" ind1="4" ind2=" ">
            <subfield code="s">1777557</subfield>
            <subfield code="u">http://zaguan.unizar.es/record/79356/files/texto_completo.pdf</subfield>
            <subfield code="y">Postprint</subfield>
        </datafield>
        <datafield tag="856" ind1="4" ind2=" ">
            <subfield code="s">281974</subfield>
            <subfield code="u">http://zaguan.unizar.es/record/79356/files/texto_completo.jpg?subformat=icon</subfield>
            <subfield code="x">icon</subfield>
            <subfield code="y">Postprint</subfield>
        </datafield>
        <datafield tag="909" ind1="C" ind2="O">
            <subfield code="o">oai:zaguan.unizar.es:79356</subfield>
            <subfield code="p">articulos</subfield>
            <subfield code="p">driver</subfield>
        </datafield>
        <datafield tag="951" ind1=" " ind2=" ">
            <subfield code="a">2020-01-17-21:59:13</subfield>
        </datafield>
        <datafield tag="980" ind1=" " ind2=" ">
            <subfield code="a">ARTICLE</subfield>
        </datafield>
    </record>

    
</collection>