[HTML][HTML] The Cycladic Blueschist Unit of the Hellenic subduction orogen: Protracted high-pressure metamorphism, decompression and reimbrication of a diachronous …
We discuss the assembly and tectonochronology of the Cycladic Blueschist Unit (CBU) in
the central Aegean Sea region, Greece, as a composite, subduction-related, high-pressure …
the central Aegean Sea region, Greece, as a composite, subduction-related, high-pressure …
Collision leading to multiple-stage large-scale extrusion in the Qinling orogen: insights from the Mianlue suture
The geologic framework of the Phanerozoic Qinling–Dabie orogen was built up through two
major suturing events of three blocks. From north to south these include the North China …
major suturing events of three blocks. From north to south these include the North China …
Map view restoration of Aegean–West Anatolian accretion and extension since the Eocene
The Aegean region (Greece, western Turkey) is one of the best studied continental
extensional provinces. Here, we provide the first detailed kinematic restoration of the …
extensional provinces. Here, we provide the first detailed kinematic restoration of the …
Disruption of the Hellenic arc: Late Miocene extensional detachment faults and steep Pliocene‐Quaternary normal faults—Or what happened at Corinth?
Extensional faults exposed in the Peloponnesus and mainland Greece, most of which are
described here for the first time, record a transition from regional extension of the Aegean …
described here for the first time, record a transition from regional extension of the Aegean …
Paleomagnetic Evidence for Pre‐21 Ma Independent Drift of South Sardinia From North Sardinia‐Corsica:“Greater Iberia” Versus Europe
It is unanimously acknowledged that the Corsica‐Sardinia microplate rotated
counterclockwise (CCW) by 40–50° between 21 and 15 Ma, synchronous with Liguro …
counterclockwise (CCW) by 40–50° between 21 and 15 Ma, synchronous with Liguro …
Formation of basins and mountain ranges in Attica (Greece): The role of Miocene to Recent low-angle normal detachment faults
In seismically active regions, active low-angle detachment faults are probably more frequent
as is commonly thought and may play an important but still underestimated role in the …
as is commonly thought and may play an important but still underestimated role in the …
Active faulting on the island of Crete (Greece)
In order to characterize and quantify the Middle–Late Quaternary and ongoing deformation
within the Southern Aegean forearc, we analyse the major tectonic structures affecting the …
within the Southern Aegean forearc, we analyse the major tectonic structures affecting the …
Postcollisional contractional and extensional deformation in the Aegean region
In the Aegean area, distinct fault patterns with their associated stress regimes are evidenced
along a curved convergent plate boundary. In this article, we analyze and review late …
along a curved convergent plate boundary. In this article, we analyze and review late …
Strain partitioning along terrane bounding and intraterrane shear zones: constraints from a long-lived transpressional system in West Gondwana (Ribeira Belt, Brazil)
Shear zones are zones of localized high strain accommodating differential motion in the
lithosphere and impacting the crustal rheology and deformational history of orogenic belts …
lithosphere and impacting the crustal rheology and deformational history of orogenic belts …
Miocene postorogenic extension of the Eocene synorogenic imbricated Hellenic subduction channel: New constraints from Milos (Cyclades, Greece)
The island of Milos is part of the South Aegean volcanic arc. The volcanic processes on
Milos, which started ca. 3.5 Ma, have been studied in detail, but the limited outcrops of …
Milos, which started ca. 3.5 Ma, have been studied in detail, but the limited outcrops of …