File:Paléogéo. Callovien sup..jpg

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Français : Au Callovien sup. émersion de la plate-forme externe et transgression maximum de la formation des "Couches à Mytilus" calcaires (biozone IIB) sur la terre briançonnaise au sud. Ennoiement généralisé à l'Oxfordien moyen (ammonites, protoglobigérines) à la suite d'une élévation du niveau marin (?). Septfontaine (1984).
English: Emersion of the external platform during the Callovian and max. transgression of the "Mytilus" formation on the karstified briançonnais domain to the south. Drowning of the platform during middle Oxfordian times (ammonites, protoglobigerinids), high sea-level ?). Septfontaine (1984).
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Author Septfontaine

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current13:09, 14 October 2011Thumbnail for version as of 13:09, 14 October 2011950 × 665 (103 KB)Septfontaine (talk | contribs)

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