Results 11 to 20 of about 17,905 (130)
The nature and origin of magnetic anomalies over the Gölcük caldera; Isparta; South-Western Turkey [PDF]
For the first time; ground magnetic survey was performed which data were inverted by means of total horizontal derivative; horizontal gradient analytic signal; and hyperbolic tilt angle techniques to identify subsurface volcanic structures around ...
M. N. Dolmaz +4 more
doaj +4 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
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
Lithostratigraphy and Sedimentological Characteristics of the Calciturbidites of the Babadağ Formation-Tavas Nappe (SW Turkey) [PDF]
The Lycian Nappes contain slices of ophiolites and sedimentary rocks of various ages that crop out in SW Turkey. They evolved and were emplaced under the effect of the Late CretaceousMiocene compressional regime.
Basiru Mohammed Kore +3 more
core +3 more sources
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
Late Palaeozoic extensional volcanism along the northern margin of Gondwana in southern Turkey: implications for Palaeotethyan development [PDF]
The Late Palaeozoic-Early Mesozoic Tethyan development of the Eastern Mediterranean region remains debatable, especially in Turkey, where alternative northward and southward subduction hypotheses are proposed.
Parlak, Osman +2 more
core +1 more source

