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<identifier>oai:HAL:hal-00411860v1</identifier>
<datestamp>2018-01-11</datestamp>
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<title lang=en>Tectonic control on diagenesis in a foreland basin: combined petrologic and thermochronologic approaches in the Gres d'Annot basin (Late Eocene-Early Oligocene, French-Italian external Alps)</title>
<creator>Labaume, Pierre</creator>
<creator>Jolivet, Marc</creator>
<creator>Souquiere, F.</creator>
<creator>Chauvet, Alain</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>
<source>ISSN: 0954-4879</source>
<source>EISSN: 1365-3121</source>
<source>Terra Nova</source>
<publisher>Wiley-Blackwell</publisher>
<identifier>hal-00411860</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00411860</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00411860</source>
<source>Terra Nova, Wiley-Blackwell, 2008, 20 (2), pp.95-101. 〈10.1111/j.1365-3121.2008.00793.x〉</source>
<identifier>DOI : 10.1111/j.1365-3121.2008.00793.x</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/j.1365-3121.2008.00793.x</relation>
<language>en</language>
<subject lang=en>Massif western alps</subject>
<subject lang=en>alpine</subject>
<subject lang=en>sedimentation</subject>
<subject lang=en>calibration</subject>
<subject lang=en>France</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<subject>[SDU.STU.PE] Sciences of the Universe [physics]/Earth Sciences/Petrography</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Combined petrographic study and apatite fission track analysis (apatite FTA) across the Gres d'Annot basin document maximum temperatures reached by this turbiditic sandstone formation, from around 60 degrees C at the SW basin margin up to around 200 degrees C below the Penninic frontal thrust, in relation to burial below the front of Alpine nappes. Increasing diagenetic grade across the basin is primarily expressed by the development of silica transfer by pressure solution and correlated porosity loss. We infer the nappe thickness profile, from the nappe front in the SW up to around 8-10 km in the NE. Apatite FTA dates exhumation of the Gres d'Annot during the Late Miocene, in relation to thrusting of the underlying Argentera and Barrot Palaeozoic massifs. This study illustrates the influence of thrust front propagation on foreland basin diagenesis and exhumation, and highlights potential implications for the evolution of sediment reservoir properties in this context.</description>
<date>2008</date>
</dc>
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