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

Deep-marine clastic turbidite beds commonly occur in the Southern Apennines and record
the main tectonic phases associated with the structural evolution of the area. Based on …

Carboniferous sandstone within the Paleo-Mesomediterranean Domain (Malaguide
Subdomain), in southern Spain, represents a key detrital mode within the sedimentary …

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 present work deals with the provenance of lower-middle Jurassic successions
belonging to the External Prerif Foreland basin, which remains till now misunderstood and …

Assessing the size of a former ocean of which only remnants are found in mountain belts is
challenging but crucial to understanding subduction and exhumation processes. Here we …

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 …

Petrography and geochemistry of sandstone for the lower Oligocene volcanic-related
sandstones of Abbasabad-Kahak area, NE Iran, are detected to decipher provenance …