{"refrec":{"BRefID":219097,"RR":"<b>Errera, M; Mamet, B.; Sartenaer, P.</b> (1972). Le Calcaire de Givetien à Givet. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 48(1)</i>: 59 pp 6 figs 2 pls","BEntID":210836,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 48(1)</i>: 59 pp 6 figs 2 pls","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Errera, M; Mamet, B.; Sartenaer, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Errera, M <i>et al.</i>","Englishabstract":"The authors recount the original definitions and the evolution of the conceptions of the Giuet Limestone and the Givetian at Givet. In order to end the existing confusion they define a Givet Group composed of three formations, which are, from base to top : Trois-Fontaines, Mont d'Haurs and Fromelennes Formations.Each of these formations corresponds to a third order positive-negative bisequence (marine facies - sabkha - marine facies), while second order sequences permit the recognition of thirty-two major phases which indicate the following environments : detrital and non-turbulent in the euphotic zone, reef, lagoon and of sabkha; minor first order sequences are recognized in those major phases.As for the Givetian, the authors make suggestions to be eventually examined by international bodies","AbstractOtherLang":"Les auteurs rappellent, en partant des définitions originelles, l'évolution des conceptions relatives au Calcaire de Givet et au Givetien à Givet. Dans le but de mettre fin à la confusion existante, ils définissent un Groupe de Givet composé de trois formations qui sont, de la base au sommet : les Formations de Trois-Fontaines, du Mont d'Haurs et de Fromelennes.Chacune de ces formations correspond à une biséquence positive-négative de troisième ordre (faciès marin - sabkha - faciès marin), tandis que les séquences de deuxième ordre permettent de reconnaître trente-deux phases majeures traduisant les milieux suivants : détritique et non turbulent dans la zone euphotique, récifal, lagunaire et de sabkha; des séquences mineures de premier ordre sont reconnues dans les phases majeures.Pour le Givetien les auteurs font des suggestions susceptibles d'être examinées par les instances internationales.","BibLvlCode":"AS","StandardTitle":"Le Calcaire de Givetien à Givet","OrigTitleLangCode":"fr","OrigTitleLangCodeExtended":"fre","OrigTitleLangID":22,"DateLastModified":{"date":"2025-07-02 08:33:14.980000","timezone_type":1,"timezone":"+00:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1972,"MonPub":null,"DateUpdate":"2013-12-02","DateCreate":"2012-10-17","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":219097,"PubliDate":1972,"Pagination":"59 pp 6 figs 2 pls","XtraPublOfAnaID":null,"ISBN":null,"Volume":"48","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":64308,"SerRR":"Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. 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