@article{10272/8366,
year = {2007},
url = {http://hdl.handle.net/10272/8366},
abstract = {The lower Paleogene stratigraphic successions of the Talembote upper Ghomaride Unit represent an interval
of age going from the (middle?) Ilerdian to the early Bartonian, showing a transgressive sequence interrupted
by intermittent sedimentary gaps, which are indicated by surfaces of discontinuity. These sediments
correspond essentially to carbonatic facies with benthic foraminifers deposited in a shallow platform that
was maintained probably until the late Lutetian. The abrupt rupture of this platform allowed, during the
early Bartonian, sedimentation of pelagic to hemipelagic facies in a bathyal sedimentary environment.
Later, the sudden interruption of the sedimentation in the early Bartonian, indicated by a paleosoil, may
be better explained by tectonic reason than eustatism taking into account many actual geodynamic
reconstructions},
title = {La serie paleógena de la unidad superior del Gomáride en Talembote (Rif Interno, Marruecos)},
title = {The Paleogene successions in the upper Ghomaride unit in Talembote (Internal Rif, Morocco)},
author = {Hlila, Rachid and Maaté, Ali and Sanz de Galdeano, Carlos and Serra Kiel, Josep and Serrano Lozano, Francisco and El Kadiri, Khalil},
}