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Français : Séquence virtuelle émersive de comblement "shallowing upward sequence" caractéristique des dépôts carbonatés du Lias moyen sur la marge sud de la Téthys, valable pour le Maghreb, la plaque apulienne (Italie, Yougoslavie) jusqu'à la péninsule du Musandam en Oman et les régions himalayennes... Les fossiles (lithiotidés, foraminifères, algues) sont identiques tout au long de la marge sur plus de 10.000 km ! Illustration en photos ci-dessous. Plus d'info. sur www.palgeo.ch/publications
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Author Septfontaine

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26 March 2008

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current13:03, 6 October 2011Thumbnail for version as of 13:03, 6 October 20111,002 × 1,467 (424 KB)Septfontaine

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