Results 1 to 10 of about 239 (95)
The Lycian nappes lying on top of the para–autochthonous metamorphosed Menderes and unmetamorphosed Bey Dağları successions in SW Anatolia belong to the Tauride segment of the Anatolide–Tauride Block.
Bilal Sári
exaly +9 more sources
Late Triassic ostracods from the Lycian Nappes, southwestern Turkey: implications on taxonomy and palaeobiogeographical distribution [PDF]
The first ostracods known from the Lycian Nappes in southwestern Turkey are here reported, adding to the scientific understanding of marine ostracods during the Cordevolian, early Carnian, Late Triassic.
Marie-Béatrice Forel
exaly +6 more sources
On the geoarchaeology of Limyra (SW Anatolia)-new insights into the famous Lycian city and its environs. [PDF]
Abstract Geoarchives in ancient settlement sites and their environs bear valuable information about Holocene landscape evolution and human–environment interactions. During the last six millennia, sea‐level and coastline changes have had a significant impact on coastal settlements, some of which even had to be relocated.
Stock F +4 more
europepmc +2 more sources
Paleoseismological features and tectonic setting of the Fethiye-Burdur fault zone (SW Turkey) [PDF]
The Fethiye‐Burdur fault zone is not a single line. Still, it consists of discontinuous northeasterly trending fault segments developed parallel to each other between the Gulf of Fethiye and Burdur Lake.
Sari Coşkun +5 more
doaj +1 more source
Thrace Basin—An Oligocene Clastic Basin Formed During the Exhumation of the Rhodope Complex
Abstract Some orogenic sedimentary basins are difficult to assign to a particular category. An example is the hydrocarbon‐bearing Thrace Basin in the northern Aegean. It has more than 9‐km‐thick Cenozoic clastic sediment, and is spatially associated with the Rhodope metamorphic core complex in the west, and with the Tethyan subduction‐accretion ...
Aral I. Okay +7 more
wiley +1 more source
Abstract The southwestern margin of the Central Anatolian Plateau corresponds to the upper crust of the subduction between African and Anatolian plates, with a high relief of up to 2 km. This mountainous region has distinctive geomorphological features and presents a unique setting to investigate the mechanism of orogenic plateau margin development ...
Tunahan Aykut +2 more
wiley +1 more source
Abstract We report four K‐Ar fault‐gouge and eight U‐Pb calcite ages from the high‐pressure Phyllite‐Quartzite Unit (PQ) and the overlying, strongly thinned non‐high‐pressure Tripolitza and Pindos units of western Crete, Greece. We relate consistent 26–21 Ma fault‐gouge ages to a discrete top‐to‐the‐S, brittle‐ductile, contractional shear zone (Intra ...
Uwe Ring +5 more
wiley +1 more source
Seismic‐stratigraphic analysis of Resolution Guyot as a prime examples of the Cretaceous Mid‐Pacific atolls revealed controls from the Cretaceous eustasy on the evolution and karstification of the Cretaceous Mid‐Pacific atolls along with other factors including changes in subsidence and production rates and later magmatic activity(ies). Abstract Atolls
Mahmoud S. El‐Yamani +2 more
wiley +1 more source
Applying an integrated methodology, including petrography, mercury injection capillary pressure (MICP), laboratory nuclear magnetic resonance (NMR) and X‐ray computed tomography (XCT), on continental spring carbonate reservoir analogue samples is a prerequisite to understanding plug scale porosity and permeability heterogeneities.
Jeroen Soete +8 more
wiley +1 more source
Abstract We report the results of a field study on Sikinos Island in the Aegean extensional province of Greece and propose a hinge zone controlling incipient bivergent extension in the southern Cyclades. A first deformation event led to top‐S thrusting of the Cycladic Blueschist Unit (CBU) onto the Cycladic basement in the Oligocene. The mean kinematic
Uwe Ring, Johannes Glodny
wiley +1 more source

