High amounts of Chattian-Langhian orogenic magmatism have generated volcaniclastic deposits that are interbedded within the penecontemporaneous sedimentary marine successions in several central-western peri-Mediterranean chains. These deposits are widespread in at least 41 units of different basins located in different geotectonic provinces: (1) the Africa-Adria continental margins (external units), (2) the basinal units resting on oceanic or thinned continental crust of the different branches of the western Tethys, (3) the European Margin (external units), and (4) the Western Sardinia zone (Sardinia Trough units). The emplacement of volcaniclastic material in marine basins was controlled by gravity flows (mainly turbidites; epiclastites) a...
In recent years, a team of Italian and foreign researchers have carried out detailed multidisciplina...
The latest Carboniferous to lower Permian volcanism of the southern Variscides in Sardinia developed...
The genetic relationships between orogenic and anorogenic magmatic cycles have been investigated in...
High amounts of Chattian-Langhian orogenic magmatism have generated volcaniclastic deposits that are...
In the central-western peri-Mediterranean chains, a consistent latest Chattian-Langhian orogenic cal...
In the central-western peri-Mediterranean chains, a consistent latest Chattian-Langhian orogenic cal...
The Early Miocene Bisciaro Fm., a marly limestone succession cropping out widely in the Umbria–Romag...
The Mediterranean area is one of the most intriguing places on Earth where geodynamics and volcanoes...
Abstract Volcaniclastic debris-rich formations, characterising the Troina–Tusa Unit in the Sicilia...
The long migration of the Balearic Arc (Alpine-Apennine and Alpine- Maghrebian belts) in the Early-...
The genetic relationships between orogenic (i.e. subduction related) and anorogenic (i.e. intra-plat...
The Neogene to Present geodynamic and magmatological evolution of the western Mediterranean area may...
The second stage of the Sardinian Rift: volcanism and evolution of Ardara-Chilivani and Bonorva sub-...
Two volcaniclastic deposits, ROC and SBA, in the Oligo-Miocene succession of the Southern Apennines,...
We present a geodynamic reconstruction of the Central-Western Mediterranean and neighboring areas du...
In recent years, a team of Italian and foreign researchers have carried out detailed multidisciplina...
The latest Carboniferous to lower Permian volcanism of the southern Variscides in Sardinia developed...
The genetic relationships between orogenic and anorogenic magmatic cycles have been investigated in...
High amounts of Chattian-Langhian orogenic magmatism have generated volcaniclastic deposits that are...
In the central-western peri-Mediterranean chains, a consistent latest Chattian-Langhian orogenic cal...
In the central-western peri-Mediterranean chains, a consistent latest Chattian-Langhian orogenic cal...
The Early Miocene Bisciaro Fm., a marly limestone succession cropping out widely in the Umbria–Romag...
The Mediterranean area is one of the most intriguing places on Earth where geodynamics and volcanoes...
Abstract Volcaniclastic debris-rich formations, characterising the Troina–Tusa Unit in the Sicilia...
The long migration of the Balearic Arc (Alpine-Apennine and Alpine- Maghrebian belts) in the Early-...
The genetic relationships between orogenic (i.e. subduction related) and anorogenic (i.e. intra-plat...
The Neogene to Present geodynamic and magmatological evolution of the western Mediterranean area may...
The second stage of the Sardinian Rift: volcanism and evolution of Ardara-Chilivani and Bonorva sub-...
Two volcaniclastic deposits, ROC and SBA, in the Oligo-Miocene succession of the Southern Apennines,...
We present a geodynamic reconstruction of the Central-Western Mediterranean and neighboring areas du...
In recent years, a team of Italian and foreign researchers have carried out detailed multidisciplina...
The latest Carboniferous to lower Permian volcanism of the southern Variscides in Sardinia developed...
The genetic relationships between orogenic and anorogenic magmatic cycles have been investigated in...