{"refrec":{"BRefID":199307,"RR":"<b>Van Vliet-Lanoë, B.; Mansy, J.-L.; Henriet, J.-P.; Laurent, M.; Trentesaux, A.; Vidier, J.-P.</b> (2003). Une inversion tectonique cénozoïque par étapes: le Pas de Calais, <b><i>in</i></b>: ASF (Ed.) <i>9ème Congrès Français de Sédimentologie. Bordeaux, 14-15-16 octobre 2003: Livre des résumés. Publications ASF,</i> 38: pp. 515","BEntID":191611,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: ASF (Ed.) <i>9ème Congrès Français de Sédimentologie. Bordeaux, 14-15-16 octobre 2003: Livre des résumés. Publications ASF,</i> 38: pp. 515","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Van Vliet-Lanoë, B.; Mansy, J.-L.; Henriet, J.-P.; Laurent, M.; Trentesaux, A.; Vidier, J.-P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Van Vliet-Lanoë, B. <i>et al.</i>","Englishabstract":"Le Boulonnais est un dôme où s'emboite un paléo-golfe marin déjà partiellement excavé pendant l’Eocène supérieur, dôme conséquence d'une inversion tectonique dès l'Eocène moyen. De nouvelles données sédimentaires et paléopédologiques recueillies à l'intérieur du Boulonnais et au niveau des Fosses Dangeard permettent de mieux comprendre son inversion par étape en les associant aux données sismiques existantes. Le détroit du Pas de Calais a probablement été ouvert au Lutétien, pendant une partie de l'Oligocène et au Néogène supérieur: les faunes oligocènes et pliocènes sont identiques de part et d'autre du détroit. Il s'est refermé épisodiquement pour des raisons tectoniques et eustatiques, à l'Oligocène final, certainement au Miocène inférieur et moyen, et à partir du Quatemaire ancien pour n'être réouvert que tardivement lors du Dernier Interglaciaire. Les réouvertures sont en relation avec l'évolution de la Manche orientale et de son réseau de paléovallées. L'inversion du front varisque a accommodé l'essentiel du raccourcissement impose à la plate-forme occidentale de l'Europe lors de la remontée de la plaque ibérique puis, de la formation des Pyrénées. L'inversion du bassin Boulonnais-Weald est quasi-synchrone de celle des autres basins de la Manche et de la Mer du Nord. Les implications tectoniques, géomorphologiques et climatiques de cette dynamique sont discutées dans le contexte de l'Europe occidentale.","AbstractOtherLang":null,"BibLvlCode":"AMS","StandardTitle":"Une inversion tectonique cénozoïque par étapes: le Pas de Calais","OrigTitleLangCode":"fr","OrigTitleLangCodeExtended":"fre","OrigTitleLangID":22,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2003,"MonPub":null,"DateUpdate":"2011-11-29","DateCreate":"2010-10-14","SecASFANote":null,"ConfID":null,"PeerRev":null,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":199307,"PubliDate":2003,"Pagination":"515","XtraPublOfAnaID":null,"ISBN":"2-907205-37-4","Volume":"38","Issue":null,"BRefMon":199305,"BRefMonRR":"<b>ASF (Ed.)</b> (2003). 9ème Congrès Français de sédimentologie. 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