Structural organization of the Lorraine coal basin and formation of the Alsting thrust fold

De la géologie structurale à la géodynamique : un numéro thématique dédié à la contribution de l’école rennaise de tectonique - Hommage à J-P Brun, P. Choukroune et P.R. Cobbold

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Fig. 4

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(a): Wells location on the structural map. Note also the location of the different NE-SW sub-stages thickness profiles from well data. These thickness profiles are presented on Figure. The map is projected with Lambert 93 system explaining the gap of the X and Y coordinates locations. (b): Summary of the different parameters used in the seismic-to-well tie procedure. Cg (conglomerate), Cl (claystone), Co (coal), Li (limestone) and Sa (sandstone).

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