SEDIMENTOLOGIE DE FACIES DES DEPOTS TRIASIQUES DE LA REGION DE OUED EL MALEH ET ELGARA (BASSIN DE MOHAMMEDIA-BENSLIMANE-ELGARA-BERRECHID, MAROC).
- Laboratoire de Dynamique des bassins s?dimentaires et corr?lations g?ologiques, Facult? des Sciences Ben M?sik, Universit? Hassan II de Casablanca. B.P. 7955, Sidi Othmane, Casablanca, Maroc.
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The Triassic deposits of the Mohammedia-Benslimane-ElGara-Berrechidbasin have a silicoclastic and saliferous nature covered by basaltic flows. These deposits occur locally in the northern, eastern and southern parts of the basin, and plunge weakly towards the south west under cretaceous deposits. In this paper, we are interested in the Triassic outcrops at Oued El Maleh-ElGara area (central and northern part of the basin). The detailed description of the outcrops and the recognition of facies and architectural elements characteristic of the deposition environment revealed the existence of a clastic and evaporitic episode before the basalt effusion. This study has shown an important palaeoenvironmental evolution that has evolved from an alluvial fan environment (the base of the series) to a braided river environment that becomes anastomosed (middle of the series). At the end, the system moved to a coastal plain environment characterized by very fine and evaporitic deposits resulting from an installation of lacustrine and also lagoonal environments in connection with a Upper-Triassic epicontinental sea.
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[Abdelkrim Afenzar and Rachid Essamoud. (2017); SEDIMENTOLOGIE DE FACIES DES DEPOTS TRIASIQUES DE LA REGION DE OUED EL MALEH ET ELGARA (BASSIN DE MOHAMMEDIA-BENSLIMANE-ELGARA-BERRECHID, MAROC). Int. J. of Adv. Res. 5 (May). 1938-1949] (ISSN 2320-5407). www.journalijar.com
Faculté des Sciences Ben M'sik, Université Hassan II de Casablanca