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Aegean tectonics: Strain localisation, slab tearing and trench retreat
We review the geodynamic evolution of the Aegean–Anatolia region and discuss strain
localisation there over geological times. From Late Eocene to Present, crustal deformation in …
localisation there over geological times. From Late Eocene to Present, crustal deformation in …
Continental and oceanic core complexes
Core-complex formation driven by lithospheric extension is a first-order process of heat and
mass transfer in the Earth. Core-complex structures have been recognized in the continents …
mass transfer in the Earth. Core-complex structures have been recognized in the continents …
Tectonic evolution of the Gediz Graben: field evidence for an episodic, two-stage extension in western Turkey
Western Turkey is one of the most spectacular regions of widespread active continental
extension in the world. The most prominent structures of this region are E–W-trending …
extension in the world. The most prominent structures of this region are E–W-trending …
Origin of NE-trending basins in western Turkey
The origin of NE-trending basins and their relation to the E–W-trending grabens in western
Turkey have been the subject of long lasting debate. The stratigraphical and structural …
Turkey have been the subject of long lasting debate. The stratigraphical and structural …
The geological signature of a slab tear below the Aegean
In this paper we explore the geology of the Aegean region in the Miocene to identify the
geological signature of a first-order slab tear observed in all tomographic models. From 15 to …
geological signature of a first-order slab tear observed in all tomographic models. From 15 to …
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 …
Application of low-temperature thermochronometry to extensional tectonic settings
Extension and associated tectonic exhumation have been described across a diverse
spectrum of geodynamic environments, ranging from lithospheric-scale extension along …
spectrum of geodynamic environments, ranging from lithospheric-scale extension along …
Metamorphic core complexes: Windows into the mechanics and rheology of the crust
Metamorphic core complexes are products of normal-fault displacements sufficient to
exhume rocks from below the brittle–ductile transition. These faults (detachments) may …
exhume rocks from below the brittle–ductile transition. These faults (detachments) may …
What caused the denudation of the Menderes Massif: Review of crustal evolution, lithosphere structure, and dynamic topography in southwest Turkey
The deformation of Earth's lithosphere in orogenic belts is largely forced externally by the
sinking slab, but can also be driven by internal delamination processes caused by …
sinking slab, but can also be driven by internal delamination processes caused by …
The mechanical paradox of low-angle normal faults: Current understanding and open questions
Low-angle normal faults, LANF,(dip< 30°) have been proposed as key-structures for
accommodating crustal extension. In contrast, frictional fault reactivation theory predicts that …
accommodating crustal extension. In contrast, frictional fault reactivation theory predicts that …