Français : Le détritisme gréseux s'intensifie sur la plate-forme qui s'étend au nord et transgresse toujours vers le sud. Le quartz provient de l'épaulement du rift liasique. Le domaine intermédiaire carbonaté émerge (transpression) et des dépôts torrentiels (galets ronds du Dogger, voir fig. suiv., charbons) s'accumulent dans des marais maritimes, zone du Château d'Oche. Septfontaine (1984, fig. 32).
English: Detrital quartz deposits spread all over the platform, transgressive to the north and to the south. Detrital quartz comes fron the rift shoulder. Torrential river deposits (rounded jurassic limestone pebbles and boulders) on the Château d'Oche zone. Septfontaine (1984, fig.32)
to share – to copy, distribute and transmit the work
to remix – to adapt the work
Under the following conditions:
attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
share alike – If you remix, transform, or build upon the material, you must distribute your contributions under the same or compatible license as the original.