{"refrec":{"BRefID":71742,"RR":"Dupuis, C.; Steurbaut, E. (1987). Altérites, sables marins (NP8, NP9) et fluviatiles, silicification et stromatolites dans le Paléocène supérieur entre Criel et le Cap d'Ailly (Haute-Normandie). Ann. Soc. Géol. Nord 105: 233-242","BEntID":67765,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". Ann. Soc. Géol. Nord 105: 233-242","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Dupuis, C.; Steurbaut, E.","OrigTitleTranslFlag":1,"Authorstringtrunc":"Dupuis, C.; Steurbaut, E.","Englishabstract":"Along the cliffs of the Haute-Normandie, between Criel and the Cap d'Ailly, the so-called thanetian sands, lying below the Formation de Varengeville (NP11) and the sparnacian facies (french sense) remained bad known.Our study allow to define in this sands, four formations, the relationships of which are explicited.Two are marine, with a \"thanetian\" facies: the Sables de Dieppe and de Criel; the two others are continental; the Sables du Petit-Ailly are fluviatile and the Sables et Grès du Pays-de-Caux strict sense are characterised by their near-surface diagenesis.The Sables de Dieppe and the Sables de Criel being attributed respectively to the NP8 and the NP9 biozones, the tertiary succession of the Haute-Normandie is now well situated between the NP8 and NP11 zones.Thus the majn demonstrated events can be located jn the time scale:-the local end of the pedologic evolution of the chalk (NP8); the high marine relative level causing the maximum stretching of the thanetian sea at the top of the Palaeocene (NP8),-the sparnacian facies transgression (londinian transgression) coinciding with the interruption of the continental limestone leaching (after NP9).","AbstractOtherLang":"Entre Criel et le Cap d'Ailly, sous la Formation de Varengeville (NP11) et les faciès sparnaciens, les sables thanétiens, difficiles d'accès, restaient mal connus.Notre étude permet d'y définir quatre formations dont les relations mutuelles sont précisées.Deux sont marines, de faciès \"thanétien\" : les Sables de Dieppe et de Criel ; les deux autres continentales: les Sables du Petit-Ailly, fluviatiles et les Sables et Grès du Pays-de-Caux s.s., singularisés par leur diagenèse supergène.Les Sables de Dieppe étant attribués à la biozone NP8 et les Sables de Criel à la biozone NP9, la série tertiaire de Haute Normandie se trouve calée entre les biozones NP8 et NP11. Ainsi peuvent être situés dans Ie temps les principaux événements mis en évidente, entre autres: la fin locale de l'évolution pédologique du substrat crayeux (NP8);Ie haut niveau marin (relatif) marquant l’extension maximum de la mer thanétienne à la fin du Paléocène (NP8),la transgression des faciès sparnaciens (transgression londinienne) coïncidant avec la fin de Ia mobilisation continentale du calcaire (post NP9).","BibLvlCode":"AS","StandardTitle":"Altérites, sables marins (NP8, NP9) et fluviatiles, silicification et stromatolites dans le Paléocène supérieur entre Criel et le Cap d'Ailly (Haute-Normandie)","OrigTitleLangCode":"fr","OrigTitleLangCodeExtended":"fre","OrigTitleLangID":22,"DateLastModified":{"date":"2024-12-10 01:32:52.928458","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1987,"MonPub":null,"DateUpdate":"2016-02-17","DateCreate":"2005-03-21","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":71742,"PubliDate":1987,"Pagination":"233-242","XtraPublOfAnaID":null,"ISBN":null,"Volume":"105","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":71738,"SerRR":"Annales de la Société Géologique du Nord. Société Géologique du Nord: Lille. ISSN 0767-7367","StandardTitleSer":"Annales de la Société Géologique du Nord","ISSN":"0767-7367","AbbrevSer":"Ann. Soc. Géol. Nord","StandardTitleMon":null,"StartPage":233,"Pages":10,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":{"Line1":"Rue de Houdain 9","Email":null,"Line2":null,"EnvName":"Belgium"},"othpubs":null,"ownerships":null,"authors":[{"AutName":"Dupuis","Firstname":"Christian","Initials":"C.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":67765,"AutID":52066,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Steurbaut","Firstname":"Etienne","Initials":"E.","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":67765,"AutID":30006,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":3501,"InsID":null}],"mapdetails":null,"datasets":null,"monographs":null,"monparts":null,"serparts":null,"BEntOpen":null,"BEntPrivate":null,"availability":[{"BInstID":284853,"LibID":36,"BRefID":71742,"EmbargoDate":null,"FullEmbargoDate":null,"PhysMedID":16,"hasOCRd":1,"ShelfLocCode":"284853","RFID":null,"PaidValue":null,"Medium":"Server","Description":"Interne VLIZ documenten","Acronym":"VLIZ","Library":"Vlaams Instituut voor de Zee","DutchTerm":"Non-open access","URL":null,"ClassifID":228,"Classification":"Non-open access","ReqLink":1,"ClassifTypID":3,"URLLocation":"https://www.vliz.be/imisdocs/publications/","SubDir":1,"InternalReq":1,"LoggedInReq":1,"Disclaimer":"Disclaimer_VLIZ_Intern","DutchDisclaimer":"
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