{"refrec":{"BRefID":233915,"RR":"<b>Boulvain, F.; Coen-Aubert, M.</b> (2006). A fourth level of Frasnian carbonate mounds along the south side of the Dinant Synclinorium (Belgium). <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 76</i>: 31-51","BEntID":225599,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 76</i>: 31-51","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Boulvain, F.; Coen-Aubert, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Boulvain, F.; Coen-Aubert, M.","Englishabstract":"An additional level of Frasnian mounds has been recognized in the La Boverie quarry at Rochefort and in four boreholes drilled in the Nord quarry at Frasnes, on the south side of the Dinant Synclinorium. It occurs between the Arche and Lion Members belonging respectively to the Moulin Liénaux and Grands Breux Formations, in the middle part of the stage. The new name of La Boverie Member is introduced at the top of the Moulin Liénaux Fm., for the deposits lying between the Arche and Bieumont Members; the latter is the basement of the Lion mound. The same succession has been observed in the sections of Moulin Bayot close to Vodelée, in the southeastern part of the Philippeville Anticlinorium. The La Boverie Member starts with rather deep bioclastic sediments, after the collapse of the carbonate factory at the top of the Arche mound. In the upper part of the lithostratigraphic unit, there is a thin buildup characterized by relatively shallow facies. The solitary rugose corals <i>Macgeea boveriensis</i> n. sp., <i>M. socialis</i> SOSHKINA, 1939 and <i>Sinodisphyllum posterum</i> (IVANIA, 1965) collected in the lower part of the La Boverie Member are described in detail whereas the revision of <i>S. kielcense</i> (ROZKOWSKA, 1979) occurring in the Bieumont Member is also provided.","AbstractOtherLang":"Un niveau supplémentaire de monticules frasniens a été reconnu dans la Carrière de la Boverie à Rochefort et dans quatre sondages forés dans la Carrière du Nord à Frasnes. Il se trouve entre les Membres de l'Arche et du Lion appartenant respectivement aux Formations du Moulin Liénaux et des Grands Breux, dans la partie moyenne de l'étage. Le nouveau nom du Membre de La Boverie est introduit au sommet de la Formation du Moulin Liénaux, pour les dépôts situés entre les Membres de l'Arche et de Bieumont; ce dernier est le soubassement du monticule du Lion. La même succession a été observée dans les coupes du Moulin Bayot près de Vodelée, dans la partie sud-est de l'Anticlinorium de Philippeville. Le Membre de La Boverie débute par des sédiments bioclastiques, plutôt profonds après l'effondrement de la production carbonatée au sommet du monticule de l'Arche. Dans la partie supérieure de l'unité lithostratigraphique, il y a une mince bioconstruction caractérisée par des faciès relativement peu profonds. Les Rugueux solitaires <i>Macgeea boveriensis</i> n. sp., <i>M. socialis</i> SOSHKINA, 1939 et <i>Sinodisphyllum posterum</i> (IVANIA, 1965) récoltés dans la partie inférieure du Membre de La Boverie sont décrits en détail tandis que la révision de <i>S. kielcense</i> (ROZKOWSKA, 1979) présent dans le Membre de Bieumont est également proposée.","BibLvlCode":"AS","StandardTitle":"A fourth level of Frasnian carbonate mounds along the south side of the Dinant Synclinorium (Belgium)","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:32:52.928458","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Frasnian, Sedimentology, Stratigraphy, Rugose corals, Belgium","OtherDescriptors":null,"Notes":null,"AnaPub":2006,"MonPub":null,"DateUpdate":"2014-02-27","DateCreate":"2014-02-27","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":233915,"PubliDate":2006,"Pagination":"31-51","XtraPublOfAnaID":null,"ISBN":null,"Volume":"76","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":64308,"SerRR":"Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. 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