The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

We present a map that correlates tectonic units between Alps and western Turkey
accompanied by a text providing access to literature data, explaining the concepts used for …

This study presents detrital zircon U‐Pb analyses of 23 samples of the Cycladic Blueschist
Unit (CBU) from Kea, Kythnos, and Serifos islands, as well as the Lavrion Peninsula of SE …

Along the Dinaric–Hellenic orogen, the Late Jurassic–Early Cretaceous ophiolite obduction
over the Adria continental margin was sealed by sedimentation of clastic terrestrial deposits …

We have combined new titanite, zircon, and apatite fission-track and apatite [U–Th–(Sm)]/He
analyses with previously published U–Pb, Rb–Sr, and 40 Ar/39 Ar thermochronological data …

From subduction to collision and subduction again, the drivers of crustal-scale deformation
in the Hellenides-Aegean region À propos Notre revue Équipe éditoriale Les CR …

The Fanos granite occurs in the Peonias subzone of the eastern Axios-Vardar zone in
northern Greece. The Fanos granite is Late Jurassic (158±1 Ma) and trends N–S, intruding …

The Chalkidiki block is a major domain in the North Aegean that, contrary to other domains
in the region, largely escaped thermal perturbations during Tertiary extension. As a result …

The present‐day Aegean tectonic configuration is marked by the interplay between Hellenic
slab rollback and Anatolian extrusion, explaining the formation of extensional basins and …

The aim of this paper is to contribute to deciphering the evolutionary history of the
Hellenides by the study of a large sector of the chain located between the front of the …