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 …

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 …

Volcanic particles have particular geodynamic significance. Despite abundant datasets on
volcanic-derived sand (stone), the distinction between spatial and temporal distribution of …

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 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 …

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