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 …

Late to post-Variscan molassic basins of Late Pennsylvanian-Permian age are exposed in
Sardinia (Italy). Here, the compositional and stratigraphic evolution of the Mulargia …

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 …

Although tunnels are vulnerable to Permanent Ground Displacement (PGD) due to a fault
crossing, studies in assessing this intersection are limited, and most of the existing studies …

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

U–Pb spot ages on detrital zircons from turbidite quartzarenites, quartz-feldspathic and
volcaniclastic sandstones of the Tufiti di Tusa (TTF), Numidian Flysch (NF), Bifurto (BF) …

The Cenozoic sedimentary cover of the Malaguide Complex (Internal Betic Cordillera,
Spain), in the Almería and Málaga areas, consists of a suite of sedimentary successions …

A review of the paleogeographic and tectonic reconstruction of the onshore and offshore
Tunisian margin during the Cenozoic is discussed. Five unconformities (A to E) and …