{"refrec":{"BRefID":285351,"RR":"<b>Belghithi, H.; Boulvain, F.; Yaich, C.; Da Silva, A.-C.</b> (2016). Évolution des séries silicoclastiques miocènes en Tunisie centrale: cas de la coupe de Khechem El Artsouma. <i>Carnets de Géologie = Notebooks on Geology 16(23)</i>: 557-568","BEntID":277376,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Carnets de Géologie = Notebooks on Geology 16(23)</i>: 557-568","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Belghithi, H.; Boulvain, F.; Yaich, C.; Da Silva, A.-C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Belghithi, H. <i>et al.</i>","Englishabstract":null,"AbstractOtherLang":"En Tunisie, au cours du Miocène, suite à la phase de plissement NE-SW (direction atlasique), les dépôts silicoclastiques sont mis en place dans un environnement deltaïque au sud-ouest et une plate-forme marine interne au nord-est du pays. Dans cet article, nous présentons la coupe de Kechem El Artsouma, du Miocène, qui est représentative des dépôts de Tunisie centrale. Cette zone est particulièrement intéressante car elle correspond à la zone de transition entre les dépôts de delta et marins peu profonds. Nous proposons une combinaison de techniques telles que l'analyse des faciès, la susceptibilité magnétique et la mesure de la teneur en carbonate pour améliorer l'interprétation et la reconstruction des paléo-environnements et de leur évolution au cours du Miocène. Huit faciès sont identifiés, situés dans un domaine fluviatile, lagunaire et un domaine de plage. Les dépôts de la Formation Ain Grab (Langhien) sont interprétés comme déposés en phase transgressive, suivis par les dépôts de la Formation de Béglia (Serravallien) en phase régressive. La Formation de Saouaf (Serravallien-Tortonien inférieur) correspond à une phase transgressive et régressive. La coupe Kechem El Artsouma permet de proposer un modèle sédimentaire pour les dépôts du Miocène de la zone de transition en Tunisie centrale.","BibLvlCode":"AS","StandardTitle":"Évolution des séries silicoclastiques miocènes en Tunisie centrale: cas de la coupe de Khechem El Artsouma","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":"Miocene; Tunisia; sedimentary environments; facies; magneticsusceptibility","OtherDescriptors":null,"Notes":null,"AnaPub":2016,"MonPub":null,"DateUpdate":"2017-06-07","DateCreate":"2017-05-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000390796000001","VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":285351,"PubliDate":2016,"Pagination":"557-568","XtraPublOfAnaID":null,"ISBN":null,"Volume":"16","Issue":"23","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":231916,"SerRR":"Carnets de Géologie = Notebooks on Geology. 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