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File:Brèche de tempête.jpg

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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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current08:23, 8 October 2011Thumbnail for version as of 08:23, 8 October 20112,480 × 1,664 (4.35 MB)Septfontaine (talk | contribs)

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