During the Cenozoic widespread anorogenic magmatism, unrelated to recent supra-
subduction zone modification of its mantle source, developed within the Mediterranean and …

Neotethyan suprasubduction zone ophiolites represent anomalous oceanic crust developed
in older host basins during trench rollback cycles and later entrapped in orogenic belts as a …

The Aegean region is a concentrate of the main geodynamic processes that shaped the
Mediterranean region: oceanic and continental subduction, mountain building, high …

Suprasubduction zone (SSZ) ophiolites in orogenic belts represent oceanic crust generation
in subduction rollback cycles during the closing stages of basins prior to terminal continental …

The Middle Jurassic Mirdita Ophiolite in northern Albania is part of an ophiolite belt
occurring between the Apulian and Pelagonian subcontinents in the Balkan Peninsula. The …

The Lesser Caucasus occurs in the hinterland of the Arabia–Eurasia collision zone in the
broad Alpine–Himalayan orogenic belt and includes Cenozoic plutonic and volcanic …

Abstract The Tethys Ocean was compartmentalized into the Mediterranean Sea and Indian
Ocean during the early Miocene, yet the exact nature and timing of this disconnection are …

The Cenozoic history of the retreating Hellenic subduction system in the eastern
Mediterranean involves subduction, accretion, arc magmatism, exhumation, normal faulting …

In the Mediterranean area, lamproitic provinces in Spain, Italy, Serbia and Macedonia have
uniform geological, geochemical and petrographic characteristics. Mediterranean lamproites …

The origin of tsunamis in the Mediterranean region and its connected seas, including the
Marmara Sea, the Black Sea and the SW Iberian Margin in the NE Atlantic Ocean, is …