File:Paléogéo. Callovien inf..jpg
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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) |
| Date | |
| Source | Own work |
| Author | Septfontaine |
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| current | 09:25, 14 October 2011 | | 950 × 631 (128 KB) | Septfontaine (talk | contribs) |
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