A synthesis of Cenozoic detrital suites from the Internal Betic-Rif Cordilleras is discussed in
relations with major paleotectonic phases during growth of orogenic belts. The discussion …

The composition and stratigraphic relations of clastic strata in diverse sedimentary basins of
the circum-Mediterranean region reflect a complete record of provenance relations since …

ABSTRACT A broad region of Mesozoic to Cenozoic tectonism along the western and
central Circum-Mediterranean (CM) margins, from southern Spain (Betic Cordillera) to the …

The changing nature of detrital signatures in clastic wedges of the Circum-Mediterranean
orogenic systems reflect the provenance relations from different source rocks of evolving …

Two main groups of geological models presented over the last four decades on the
palaeogeographic, paleotectonic and geodynamic eo-Alpine and neo-Alpine evolution of …

The Tell-Rif (Tell in Algeria and Tunisia; Rif in Morocco) is the orogenic system fringing to
the south the West Mediterranean basins. This system comprises three major tectonic …

Abstract The West European collisional Alpine belts are the result of the inversion, initiated
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …

The Carboniferous detrital suites of the Ghomaride Subdomain (Rif Cordillera, N Morocco)
has been undertaken in order to obtain paleogeographic and paleotectonic constraints …

The widely debated late Oligocene-middle Miocene Numidian Fm (NF) consists of
supermature quartzose sediments deposited in the Maghrebian Flysch Basin (MFB) …

A study of the paleoenvironmental evolution of the middle Eocene platforms recognized in
the westernmost Tethys has been carried out in the well-exposed middle Eocene …