Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic [PDF]
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 destruction by subduction accommodating convergence between the African and ...
Gürer, Derya +7 more
core +1 more source
A Paleotectonic Atlas of the African Plate: Permian to Recent
ABSTRACT The fragmentary release of petroleum data defining the deep structure and stratigraphy of African basins has been integrated with existing literature to compile 19 tectonic maps over key geological intervals from Permian to Recent times. African plate margins range in their age of opening from Late Triassic (off Lebanon), through Early/Middle ...
Duncan S. Macgregor, Colin V. Reeves
wiley +1 more source
Exhumation Paths of High-Pressure–Low-Temperature Metamorphic Rocks from the Lycian Nappes and the Menderes Massif (SW Turkey): a Multi-Equilibrium Approach [PDF]
The Menderes Massif and the overlying Lycian Nappes occupy an extensive area of SW Turkey where high-pressure–low-temperature metamorphic rocks occur. Precise retrograde P–T paths reflecting the tectonic mechanisms responsible for the exhumation of these highpressure–low-temperature rocks can be constrained with multiequilibrium P ...
Rimmelé, G. +5 more
openaire +4 more sources
Exhumation of high-pressure rocks driven by slab rollback
International audienceRocks metamorphosed under high-pressure (HP) and ultra high-pressure (UHP) conditions in subduction zones come back to the surface relatively soon after their burial and at rates comparable to plate boundary velocities.
Brun, Jean-Pierre, Faccenna, C.
core +3 more sources
Lithospheric Unzipping Explaining Hot Orogenesis During Continental Subduction
Abstract Phanerozoic accretionary orogens typically contain upper crustal nappes derived from subducted lithosphere—oceanic or continental—that display (ultra‐)high‐pressure, low‐temperature ((U)HP‐LT) metamorphism. Surprisingly, such orogens often also contain coeval continent‐derived nappes that underwent “Barrovian” (MP‐HT) syn‐burial metamorphism ...
Douwe J. J. van Hinsbergen +2 more
wiley +1 more source
Using high-resolution stratigraphy and structural analysis to constrain a “polyphase” tectonics in wedge-top basins. Inferences from the Late Tortonian Scillato Basin (central-northern Sicily). [PDF]
The present paper aims to show, both from a stratigraphic and structural points of view, the main features of a wedge-top syntectonic basin which evolved recording polyphase and non-coaxial tectonics.
GASPARO MORTICELLI, Maurizio +1 more
core +1 more source
Cold Tectonics of Kos, Central Dodecanese: Oligocene Bivergent Extension of the Pelagonian Domain
Abstract Tectonic and lithological correlations between the Cycladic Blueschist Unit of the Aegean domain and Pelagonian domain of the western Turkey have rarely been proposed. Herein, we focus on the pre‐volcanic geology of Kos, and investigate the tectonic history of the central Dodecanese Islands and the general correlation between the two domains ...
Vincent Roche +4 more
wiley +1 more source
Eclogite and blueschist facies rocks occurring as a tectonic unit between the underlying Menderes Massif (MM) and the overlying Afyon Zone/Lycian Nappes and the Bornova Flysch Zone in western Anatolia represent the eastward continuation of the Cycladic ...
M. Çetinkaplan +4 more
semanticscholar +1 more source
Microseismic activity and fluid fault interactions: some results from the Corinth Rift Laboratory (CRL), Greece [PDF]
International audienceThe Gulf of Corinth, in western-central Greece, is one of the fastest continental rifts in theworld. In its western section near the city of Aigion, the previous work has outlined theexistence of a shallow dipping ...
Bourouis, Seid, Cornet, François Henri
core +4 more sources
Abstract Reconstructing the original geometry of a high‐pressure tectonic unit is challenging but important to understand the mechanisms of mountain building. While a single nappe is subducted and exhumed, nappe‐internal thrusts may disrupt it into several subunits.
Alexandre Peillod +11 more
wiley +1 more source

