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    <subfield code="a">10.1002/gj.2884</subfield>
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    <subfield code="2">sideral</subfield>
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    <subfield code="a">eng</subfield>
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  <datafield tag="100" ind1=" " ind2=" ">
    <subfield code="a">Calvín, P.</subfield>
    <subfield code="0">(orcid)0000-0002-4485-2139</subfield>
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  <datafield tag="245" ind1=" " ind2=" ">
    <subfield code="a">Detachment fold vs. ramp anticline: A gravity survey in the southern Pyrenean front (External Sierras)</subfield>
  </datafield>
  <datafield tag="260" ind1=" " ind2=" ">
    <subfield code="c">2017</subfield>
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  <datafield tag="520" ind1="3" ind2=" ">
    <subfield code="a">The Santo Domingo Anticline (External Sierras, Southern Pyrenees), which separates the Jaca piggyback basin from the Ebro foreland basin, is a key structure of the Pyrenees. Its geometry has been interpreted both as a detachment fold and as a hangingwall anticline associated with an underlying thrust. In this paper, we present the results from a gravity survey and 2.5D gravity modelling carried out around the Santo Domingo Anticline. Density measurements indicate a sharp density contrast between the Triassic evaporites-mudstones in the core of the anticline and the sedimentary sequence (limestones and sandstones) at its limbs. Gravity anomalies together with 2.5D gravity models allow to discern the along-strike structural changes. From east to west, we document a change from the ramp-associated fold to the detachment anticline. The capabilities and limitations of the gravimetric method for the determination of fold geometry are also discussed.</subfield>
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    <subfield code="f">Unrestricted</subfield>
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    <subfield code="9">info:eu-repo/grantAgreement/ES/MINECO/CGL2014-54118-C2</subfield>
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    <subfield code="9">info:eu-repo/semantics/openAccess</subfield>
    <subfield code="a">All rights reserved</subfield>
    <subfield code="u">http://www.europeana.eu/rights/rr-f/</subfield>
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    <subfield code="a">1.654</subfield>
    <subfield code="b">2017</subfield>
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    <subfield code="b">110 / 189 = 0.582</subfield>
    <subfield code="c">2017</subfield>
    <subfield code="d">Q3</subfield>
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    <subfield code="a">0.846</subfield>
    <subfield code="b">2017</subfield>
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  <datafield tag="593" ind1=" " ind2=" ">
    <subfield code="a">Geology</subfield>
    <subfield code="c">2017</subfield>
    <subfield code="d">Q2</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Santolaria, P.</subfield>
    <subfield code="0">(orcid)0000-0002-2408-809X</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Casas, A.M.</subfield>
    <subfield code="u">Universidad de Zaragoza</subfield>
    <subfield code="0">(orcid)0000-0003-3652-3527</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Pueyo, E.L.</subfield>
    <subfield code="u">Universidad de Zaragoza</subfield>
    <subfield code="0">(orcid)0000-0002-0504-2352</subfield>
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  <datafield tag="710" ind1="2" ind2=" ">
    <subfield code="1">2000</subfield>
    <subfield code="2">428</subfield>
    <subfield code="a">Universidad de Zaragoza</subfield>
    <subfield code="b">Dpto. Ciencias de la Tierra</subfield>
    <subfield code="c">Área Geodinámica Interna</subfield>
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  <datafield tag="773" ind1=" " ind2=" ">
    <subfield code="g">53, 1 (2017), 178-190</subfield>
    <subfield code="p">Geol. j.</subfield>
    <subfield code="t">GEOLOGICAL JOURNAL</subfield>
    <subfield code="x">0072-1050</subfield>
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