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

peer reviewed ; The revision of the geological map Aye - Marche-en-Famenne (Belgium, Wallonia, Hotton) has emphasized an important deformation structure named the Marenne Fault. This fault is clearly visible at the southeastern face of the Marenne quarry. The dating by rugose corals has allowed to define with precision the Givetian lithologic units that have been put in contact by this normal faul with a later, right-lateral strike-slip component. This fault, that may be traced over a few kilometers to the East, is probably late Hercynian, of the same type and origin as the Lamsoul Fault know... Mehr ...

Verfasser: Coen-Aubert, Marie
Barchy, Laurent
Marion, Jean-Marc
Coen, Michel
Dokumenttyp: journal article
Erscheinungsdatum: 2004
Verlag/Hrsg.: Institut royal des Sciences naturelles de Belgique
Schlagwörter: Belgium / Givetian / Rugose corals / Geological mapping / Faults / Strike-slip / Belgique / Givetien / Rugueux / Cartographie géologique / Failles / Décrochement / Physical / chemical / mathematical & earth Sciences / Earth sciences & physical geography / Physique / chimie / mathématiques & sciences de la terre / Sciences de la terre & géographie physique
Sprache: Französisch
Permalink: https://search.fid-benelux.de/Record/base-28941732
Datenquelle: BASE; Originalkatalog
Powered By: BASE
Link(s) : https://orbi.uliege.be/handle/2268/8918

peer reviewed ; The revision of the geological map Aye - Marche-en-Famenne (Belgium, Wallonia, Hotton) has emphasized an important deformation structure named the Marenne Fault. This fault is clearly visible at the southeastern face of the Marenne quarry. The dating by rugose corals has allowed to define with precision the Givetian lithologic units that have been put in contact by this normal faul with a later, right-lateral strike-slip component. This fault, that may be traced over a few kilometers to the East, is probably late Hercynian, of the same type and origin as the Lamsoul Fault know 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. ; Modernisation de la carte géologique de la Wallonie