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Evolution of a low convergence collisional orogen: a review of Pyrenean orogenesis
Marble quarries in Delos Island (Greece): a geological characterization
Passive imaging of collisional orogens: a review of a decade of geophysical studies in the Pyrénées
Cenozoic mountain building and topographic evolution in Western Europe: impact of billions of years of lithosphere evolution and plate kinematics
The role of inheritance in forming rifts and rifted margins and building collisional orogens: a Biscay-Pyrenean perspective
Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-field versus far-field interactions
Distribution and intensity of High-Temperature Low-Pressure metamorphism across the Pyrenean-Cantabrian belt: constraints on the thermal record of the pre-orogenic hyperextension rifting
Transfer zones in Mediterranean back-arc regions and tear faults
Lateral variations of pressure-temperature evolution in non-cylindrical orogens and 3-D subduction dynamics: the Betic-Rif Cordillera example
Detailed tectonic reconstructions of the Western Mediterranean region for the last 35 Ma, insights on driving mechanisms
Tectonic evolution of Leros (Dodecanese, Greece) and correlations between the Aegean Domain and the Menderes Massif
Fluid properties and dynamics along the seismogenic plate interface
Neo-Tethys geodynamics and mantle convection: from extension to compression in Africa and a conceptual model for obduction
Initiation, geometry and mechanics of brittle faulting in exhuming metamorphic rocks: insights from the northern Cycladic islands (Aegean, Greece)
From ductile to brittle, late- to post-orogenic evolution of the Betic Cordillera: Structural insights from the northeastern Internal zones
Insights from the Apennines metamorphic complexes and their bearing on the kinematics evolution of the orogen
Abstract The Apennine belt represents a typical orogenic segment of the western Mediterranean, characterized by the tectonic convergence between European and Africa plates after oceanic subduction. Both oceanic- and continent-derived metamorphic complexes, considered as the remnants of the subduction-exhumation cycle, crop out in the inner sectors of the Apennine belt, where extensional deformation has dominated since the Early Oligocene. We review the available structural, metamorphic and geochronological data coming from these metamorphic complexes in order to provide a kinematics reconstruction accounting for the tectono-metamorphic evolution of the Apennines, from oceanic subduction to final extensional reworking. During the Eocene, oceanic rocks were progressively subducted down to eclogite-facies conditions following a subduction-type metamorphic gradient. The transition from oceanic- to continental-subduction was coeval with a transition from subduction-type to Barrovian-type metamorphic gradient. Continental collision, at the Eocene–Oligocene boundary, post-dated the syn-orogenic exhumation of HP-rocks and was synchronous with the onset of post-orogenic extension in the hinterland domains. Extensional deformation migrated to the east, following the forelandward migration of the thrust system at the trench. The concomitance of extension and compression is here related to fast rollback of the subducting plate and delamination of the lithospheric mantle below the subducted continental crust. Implications on how the subduction tectonics, syn-orogenic exhumation and post-orogenic extension could have controlled the circulation of HP-rocks in the developing Apennines are also discussed.
Subduction, convergence and the mode of backarc extension in the Mediterranean region
Late Cretaceous to Paleogene post-obduction extension and subsequent Neogene compression in the Oman Mountains
Abstract In SW Turkey, Fe–Mg-carpholite has recently been recognized in the basal metasediments of the Lycian Nappes, which overthrust the Menderes Massif on its southern flank. This high-pressure–low-temperature (HP–LT) metamorphic index mineral was widely found in the Bodrum peninsula region. Our new metamorphic and structural data on similar carpholite-bearing rocks found farther north in several klippen of the Lycian Nappes located on top of the Menderes Massif show that HP–LT rocks in SW Turkey occur over a distance of >200 km in both north–south and east–west directions, thus indicating a wide HP–LT metamorphic belt. The deformation pattern from the Bodrum peninsula to Çivril, all along the contact between the Lycian Nappes and the Menderes Massif, reveals the role played by major top-to-the-NE shear zones contemporaneous with exhumation of the Lycian HP–LT rocks. This deformation shows an oblique direction of opposite shear sense relative to the earlier southward translation of the Lycian Nappes over the Menderes Massif, for which top-to-the-south displacements are preserved in the upper units of the Lycian Nappes on the Bodrum peninsula, as well as at the base of the Lycian nappe klippen located farther north. The widespread distribution of well-preserved Fe–Mg-carpholite-bearing rocks in the Lycian Nappes has implications for the geometry of the accretionary wedge responsible for HP–LT metamorphism in SW Turkey.