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<publisher>HAL CCSD</publisher>
<title lang=en>Reconstruction of low temperature (< 100 C-circle) burial in sedimentary basins: A comparison of geothermometer in the intracontinental Paris Basin</title>
<creator>Blaise, Thomas</creator>
<creator>Barbarand, Jocelyn</creator>
<creator>Kars, Myriam</creator>
<creator>Ploquin, Florian</creator>
<creator>Aubourg, Charles</creator>
<creator>Brigaud, Benjamin</creator>
<creator>Cathelineau, Michel</creator>
<creator>El Albani, Abderrazak</creator>
<creator>Gautheron, Cécile</creator>
<creator>Izart, Alain</creator>
<creator>Janots, Dominique</creator>
<creator>Michels, Raymond</creator>
<creator>Pagel, Maurice</creator>
<creator>Pozzi, Jean-Pierre</creator>
<creator>Boiron, Marie-Christine</creator>
<creator>Landrein, Philippe</creator>
<contributor>GeoRessources ; Centre National de la Recherche Scientifique (CNRS) - Université de Lorraine (UL) - Centre de recherches sur la géologie des matières premières minérales et énergétiques (CREGU) - Institut national des sciences de l'Univers (INSU - CNRS)</contributor>
<contributor>Géosciences Paris Sud (GEOPS) ; Université Paris-Sud - Paris 11 (UP11) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<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>Institut de Chimie des Milieux et Matériaux de Poitiers (IC2MP) ; Université de Poitiers - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire de géologie de l'ENS (LGE) ; École normale supérieure - Paris (ENS Paris) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Agence Nationale pour la Gestion des Déchets Radioactifs (ANDRA)</contributor>
<description>International audience</description>
<source>ISSN: 0264-8172</source>
<source>Marine and Petroleum Geology</source>
<publisher>Elsevier</publisher>
<identifier>hal-01313142</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01313142</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01313142</source>
<source>Marine and Petroleum Geology, Elsevier, 2014, 53, pp.71-87. 〈10.1016/j.marpetgeo.2013.08.019〉</source>
<identifier>DOI : 10.1016/j.marpetgeo.2013.08.019</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.marpetgeo.2013.08.019</relation>
<language>en</language>
<subject lang=en>Paris Basin</subject>
<subject lang=en> Thermal modeling</subject>
<subject lang=en> Apatite fission track</subject>
<subject lang=en> Sedimentary organic matter</subject>
<subject lang=en> Geothermometers</subject>
<subject lang=en> MagEval</subject>
<subject lang=en> Fluid inclusions</subject>
<subject lang=en> Clay minerals</subject>
<subject>[SDV.MHEP] Life Sciences [q-bio]/Human health and pathology</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The thermal evolution of sediments in the shallowest part of sedimentary basins is challenging to investigate as most of the geothermometers are at their application limits. This is typically the case of the Callovian-Oxfordian claystones at the eastern border of the Paris Basin. A recent 2000 m deep well penetrated the entire Jurassic and Triassic sedimentary series and permitted coring of sediments never reached by previous drilling in this part of the basin. Thanks to the use of several independent geothermometers (apatite fission track thermochronology, fluid inclusion microthermometry, clay mineralogy and sedimentary organic matter evolution) the burial history of the Mesozoic series has been reconstructed, modeled and calibrated using kinetic algorithms relevant to the various paleothermometers used. In addition to these conventional methods, an innovative approach was developed using the temperature-dependence of the magnetic mineral assemblage within clay-rich sediments ("MagEval"). Thermal modeling indicates that the Callovian-Oxfordian and the Lower Triassic experienced maximum burial temperatures of 50 +/- 5 C-circle and 90 +/- 10 C-circle respectively, i.e., about 25 C higher than present-day. This temperature offset implies the erosion of several hundred meters of sediments which, depending on the thermal flux and conductivity considered, most likely constituted Upper Cretaceous chalk deposits. Falling sea level resulted in the exposure and subsequent dismantling of the chalk cover at the beginning of Cenozoic times. The eastern border of the basin was then subjected to slow erosion and discrete tectonic deformation.</description>
<date>2014-05-01</date>
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