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<datestamp>2018-01-11</datestamp>
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<title lang=en>Record of enhanced late Pliocene tectono-volcanic activity in the Lesser Antilles forearc basin: Insights into the long-term behaviour of the Lesser Antilles subduction zone</title>
<creator>LETICEE, Jean-len</creator>
<creator>PHILIPPON, Melody</creator>
<creator>CORNEE, Jean-jacques</creator>
<creator>MUNCH, Philippe</creator>
<creator>De Min, Lyvane</creator>
<creator>NOURY, Mélanie</creator>
<creator>Randrianasolo, Auran</creator>
<creator>LEBRUN, Jean-frederic</creator>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Dynamique de la Lithosphere ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Geologie des Reservoirs et Ressources ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<source>ISSN: 0954-4879</source>
<source>EISSN: 1365-3121</source>
<source>Terra Nova</source>
<publisher>Wiley-Blackwell</publisher>
<identifier>hal-01571956</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01571956</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01571956</source>
<source>Terra Nova, Wiley-Blackwell, 2017, 29 (4), pp.245-252. 〈10.1111/ter.12271〉</source>
<identifier>DOI : 10.1111/ter.12271</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/ter.12271</relation>
<language>en</language>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>In this study, we investigate the Lesser Antilles forearc basin, focusing on the late Pliocene to Pleistocene sedimentary archives in order to track the occurrence of extreme events triggered by enhanced subduction-related tectono-volcanic activity. We identify late Piacenzian deposits covering a major regional erosional surface, displaying sedimentary dykes and large marine boulders embedded in a mixed continental–marine matrix, characteristic of tsunamites. We interpret this episode of platform emersion and the successive cataclysmic deposits as resulting from enhanced tectonic activity at the interface of the subduction zone, synchronous with the initiation of the Lesser Antilles volcanic arc. We then discuss the implications in terms of the mechanical behaviour of the Lesser Antilles subduction zone.</description>
<date>2017-08</date>
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