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- W5879704 abstract "L'anomalie magnetique a direction W-E se situe au-dessus du synclinal des Vieux Moulins de Thilay. Le noyau de ce synclinal est constitue par de l'Ordovicien. Les roches eruptives de Willerzie sont d'âge caledonien. La bordure meridionale de l'anticlinal de Louette St. Pierre est affectee de failles normales." @default.
- W5879704 created "2016-06-24" @default.
- W5879704 creator A5011862136 @default.
- W5879704 date "1981-06-01" @default.
- W5879704 modified "2023-09-26" @default.
- W5879704 title "Observations géologiques dans la région de Willerzie" @default.
- W5879704 hasPublicationYear "1981" @default.
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