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Remise en cause du rôle paléogéographique du horst de l'Artois à l'Yprésien inférieur. Mise en évidence de l'intervention du Môle transverse Bray-Artois = Questioning the paleogeographic influence of the Artois Horst at the Lower Ypresian: evidence in favor of the intervention of the transversal Bray-Artois High
Dupuis, C.; Deconinck, J.; Roche, E. (1984). Remise en cause du rôle paléogéographique du horst de l'Artois à l'Yprésien inférieur. Mise en évidence de l'intervention du Môle transverse Bray-Artois = Questioning the paleogeographic influence of the Artois Horst at the Lower Ypresian: evidence in favor of the intervention of the transversal Bray-Artois High. C. r. Acad. sci., Sér. 2 Méc. phys. chim. sci. univers sci. Terre 298(2): 53-56
In: Comptes Rendus de l'Académie des Sciences. Série 2, Mécanique, Physique, Chimie, Sciences de l'Univers, Sciences de la Terre. Gauthiers-Villars: Montrouge. ISSN 0764-4450, more
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    Marine/Coastal
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Abstract
    The discovery of a formation similar to London Clay and Ieper Clay south of the Artois horst leads us to minimize its paleogeographic influence in favour of transversal structures. The "Artois Axis", at the lower Ypresian, cannot be considered any longer as a main boundary between the Paris Basin and the nordic Basin.
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