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            <title xml:lang="en">Geodynamic evolution of the Berrechid-ElGara-BenSlimane triassic basin (north-western Meseta, Morocco): Depositional dynamics and geometry of sedimentary bodies</title>
            <title xml:lang="fr">Évolution géodynamique du bassin triasique de Berrechid-ElGara-BenSlimane : Dynamique sédimentaire et géométrie des dépôts (Méseta nord occidentale, Maroc)</title>
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                <title xml:lang="en">Geodynamic evolution of the Berrechid-ElGara-BenSlimane triassic basin (north-western Meseta, Morocco): Depositional dynamics and geometry of sedimentary bodies</title>
                <title xml:lang="fr">Évolution géodynamique du bassin triasique de Berrechid-ElGara-BenSlimane : Dynamique sédimentaire et géométrie des dépôts (Méseta nord occidentale, Maroc)</title>
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                <term xml:lang="en">volcano-sedimentary series</term>
                <term xml:lang="en">Morocco</term>
                <term xml:lang="en">north-western Meseta</term>
                <term xml:lang="en">late Triassic-lower Liassic</term>
                <term xml:lang="en">geodynamic evolu-tion</term>
                <term xml:lang="en">geometry of sedimentary bodies</term>
                <term xml:lang="en">depositional systems</term>
                <term xml:lang="fr">Méséta nord occidentale</term>
                <term xml:lang="fr">Maroc</term>
                <term xml:lang="fr">Trias supérieur-Lias inférieur</term>
                <term xml:lang="fr">évolution géodynamique</term>
                <term xml:lang="fr">géométrie des corps sédimentaires</term>
                <term xml:lang="fr">systèmes de dépôt</term>
                <term xml:lang="fr">série volcano-sédimentaire</term>
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              <p>The volcano-sedimentary series of the Berrechid-ElGara-BenSlimane Triassic onshore oriented NNE-SSW in the north-western Meseta, is studied from data collected within outcrops and several boreholes. The study of depositional sequences allowed the distinction of five depositional systems, which follow one another in time. As well, the study of spatial and vertical distributions of these sequences determines the geometry of sedimentary bodies, inferred from analysis of isopach maps and maps of facies distribution. Thus, the adopted approach permitted to suggest the dynamics of this basin in relationship with the central Atlantic early rifting during the late Triassic-lower Liassic period.</p>
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              <p>La série volcano-sédimentaire, du bassin triasique de Berrechid-ElGara-BenSlimane de direction NNE-SSW dans la Méseta nord occidentale, est étudiée à partir des données de terrain et de nombreux sondages. L'étude faciologique des dépôts a permis la distinction de cinq systèmes de dépôt successifs dans le temps. De même les variations spa-tiales et verticales des séquences de dépôt déterminent la géométrie des corps sédimentaires déduite à partir d'une cartographie de ces séquences. Ainsi l'approche adoptée a permis de retracer la dynamique du bassin, en liaison avec le début de l'ouverture de l'Atlantique central, au cours du Trias supérieur-Lias inférieur.</p>
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