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    <titleInfo>
      <title>Reappraisal of Variscan tectonics in the southern French Massif Central</title>
    </titleInfo>
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      <namePart type="family">Chardon</namePart>
      <namePart type="given">Dominique</namePart>
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    <name type="personnal">
      <namePart type="family">Aretz</namePart>
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    <name type="personnal">
      <namePart type="family">Roques</namePart>
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    <abstract>The comprehensive kinematic analysis of the Variscan fold nappes and associated wildflysch in the Southeastern Montagne Noire shows that the nappes were thrust northeastwardly along the Cevennes fault as a result of strike-slip-dominated sinistral transpression between 340 and 323 Ma. Macro- and map-scale recumbent folding and nappe stacking were achieved by ENE-directed, strike-parallel thrust shearing. The recumbent folds evolved into sheath folds by interplay of continued strike-parallel thrust shearing and strike-normal shortening manifested by north-verging folds that grew during wildflysch sedimentation. These results call for a tectonic reassessment of the southern side of the Variscides. The foreland basin was decoupled from the hinterland along orogen-scale sinistral fault(s) trending at a high angle to the orogenic trend, which interacted with a variety of hinterlandward thrust systems. The shift from sinistral transpression to dextral transtension along the Cevennes fault after 317 Ma accompanied the closure of the Iberian-Armorican syntax by accommodating northeastward escape and gravitational collapse of the northern limb of the syntax. These results illustrate the impact of the shift from plate convergence-controlled to escape-controlled kinematics on shear sense reversal and lower crust exhumation along long-lived strike-slip fault systems.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject>
      <topic>Nappe tectonics</topic>
      <topic>Sheath fold</topic>
      <topic>Transpression</topic>
      <topic>Wildflysch</topic>
      <topic>Montagne Noire</topic>
      <topic>Cevennes fault</topic>
      <topic>Iberian-Armorican syntax</topic>
    </subject>
    <subject authority="local">
      <geographic>FRANCE</geographic>
      <geographic>MASSIF CENTRAL</geographic>
      <geographic>MONTAGNE NOIRE</geographic>
      <geographic>CEVENNES</geographic>
    </subject>
    <classification authority="local">064</classification>
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      <titleInfo>
        <title>Tectonophysics</title>
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      <part>
        <detail type="volume">
          <number>787</number>
        </detail>
        <extent unit="pages">
          <list> art. 228477 [16 p.]</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2020</dateIssued>
      </originInfo>
      <identifier type="issn">0040-1951</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010078208</identifier>
    <identifier type="doi">10.1016/j.tecto.2020.228477</identifier>
    <identifier type="issn">0040-1951</identifier>
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