{"refrec":{"BRefID":233771,"RR":"<b>Barchy, L.; Coen-Aubert, M.; Marion, J.-M.; Coen, M.</b> (2004). Mise en évidence de la Faille de Marenne sur la carte géologique Aye - Marche-en-Famenne = Highlighting of the Marenne Fault on the geological map Aye - Marche-en-Famenne. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 74-suppl.</i>: 59-71","BEntID":225456,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 74-suppl.</i>: 59-71","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Barchy, L.; Coen-Aubert, M.; Marion, J.-M.; Coen, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Barchy, L. <i>et al.</i>","Englishabstract":"The revision of the geological map Aye - Marche-en-Famenne has emphasized an important deformation structure that we have named the Marenne Fault. This fault is now clearly visible at the southeast face of the Marenne quarry. The dating by rugose corals has allowed us to define with precision the Givetian lithologic units which have been put in contact by this normal fault with a later, right-lateral strike-slip component. To the east, the Marenne Fault may be traced over a distance of 4 km, as far as the Ourthe valley, to the south of Hotton where its stratigraphic displacement is about 226 m. More generally, the Marenne Fault is probably late Hercynian, of the same type and origin as the Lamsoul Fault known to the south of Marche-en-Famenne. It seems to form part of a family of faults which are regularly observed on the south side of the Dinant Synclinorium.","AbstractOtherLang":"La révision de la carte géologique Aye - Marche-en-Famenne a mis en évidence un important accident tectonique que nous avons dénommé Faille de Marenne. Celle-ci est actuellement bien visible au front sudest de la Carrière de Marenne. Les datations par les Rugueux nous ont permis de définir avec précision les unités lithologiques du Givetien mises en contact par cette faille normale à composante décrochante dextre, postérieure. Vers l'est, la Faille de Marenne a pu être suivie sur une distance de 4 km, jusque dans la vallée de l'Ourthe, au sud de Hotton où son rejet stratigraphique est d'environ 226 m. Plus généralement, la Faille de Marenne est probablement tardi-hercyniennne, du même type et de même origine que la Faille de Lamsoul connue au sud de Marche-en-Famenne. Elle semble faire partie d'une famille de failles que l'on retrouve régulièrement au bord sud du Synclinorium de Dinant.","BibLvlCode":"AS","StandardTitle":"Mise en évidence de la Faille de Marenne sur la carte géologique Aye - Marche-en-Famenne = Highlighting of the Marenne Fault on the geological map Aye - Marche-en-Famenne","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Belgium, Givetian, Rugose corals, Geological mapping, Faults","OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2014-02-20","DateCreate":"2014-02-20","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":233771,"PubliDate":2004,"Pagination":"59-71","XtraPublOfAnaID":null,"ISBN":null,"Volume":"74-suppl.","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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