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Toggle navigation. Have you forgotten your login? Hide details. Abstract : The Aptian-Early Albian interval of the southern Tethyan margin is poorly understood since sedimentary successions are frequently incomplete and dating is difficult. The facies and depositional environments of the Aptian-Early Albian rocks are identified based on their lithology, sedimentary structures, fossil content and microfacies. These allowed to identify 1 four types of key surfaces related subaerial or submarine erosion, 2 four sedimentary carbonated facies in the Aptian corresponding to outer to inner ramp depositional environments, and 3 four Early Albian sedimentary facies, represented by sandstones and shales, of basin to middle ramp depositional setting. These facies reflect deposition in adjacent and gradational paleoenvironments. The Aptian-Early Albian stratigraphic interval of the EAB, has been subdivided into two major cycles, floored by two major erosional surfaces.
Ces documents sont reproduits dans les figures 1 et 2. Above, longitudinal profile along the E-W trench of ; between points 2 and 3, the stratigraphy recorded here by Delporte is identical to that schematically illustrated in the subsequently excavated palier sud cf. On ne sait pas non plus pourquoi la monographie Delporte n. La description de la stratigraphie et des objets recueillis au cours de ses fouilles est faite par F. Surmely et A. Mellars et al. Ils se trompent.
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