Brèche_de_tempête.jpg
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Summary
| Description |
Français :
Brèche de tempête au sommet d'une séquence régressive métrique. Les plaquettes dolomitiques stromatolitiques sont disloquées puis déplacées à la surface du rivage par les vagues et les courants débordant des chenaux sur la zone supratidale. Haut Atlas, Maroc. Voir Septfontaine (1985): Milieux de dépôts et foraminifères (lituolidés) de la plate-forme carbonatée du Lias oyen au Maroc.- Rev. de Micropal. 28/4, 265-289, ou www.palgeo.ch/publications.
Ænglisc:
Tempestite breccia on the surface of a regressive metric sequence; the dolomitic and stromatolitic elements are dislocated and reworked by hurricane waves and currents on the supratidal zone temporarily drowned. High Atlas, Morroco. See also www.palgeo.ch/publications
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| Date | |
| Source | Own work |
| Author | Septfontaine |
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