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Plate tectonics and biogeographical patterns of the Pseudophoxinus (Pisces : Cypriniformes) species complex of central Anatolia, Turkey
(ACADEMIC PRESS INC ELSEVIER SCIENCE, 2004)
We investigated the phylogenetic relationships of Pseudophoxinus (Cyprinidae: Leuciscinae) species from central Anatolia, Turkey to test the hypothesis of geographic speciation driven by early Pliocene orogenic events. We ...
Anatoliacodium gen. nov (Halimedaceae, Green algae) from the Ilerdian-Cuisian in the Eskisehir region (Western Central Turkey)
(SLOVAK ACAD SCIENCES GEOLOGICAL INST, 2009)
A new genus Anatoliacodium (Halimedaceae, Green algae) is described from the Ilerdian-Cuisian shallow-water sediments of Eskisehir region, central-western Turkey. These sequences consist of limestones, clayey limestones, ...
Kinematics of the East Anatolian Fault Zone between Turkoglu (Kahramanmaras) and Celikhan (Adiyaman), eastern Turkey
(TERRA SCIENTIFIC PUBL CO, 2006)
In this study we determined the stress regime acting along the East Anatolian Fault Zone between Turkoglu (Kahramanmaras) and Celikhan (Adiyaman), from the Neocene to present-day, based on the inversion of striations ...
Neotectonic deformation in the western sector of tectonic escape in Anatolia: palaeomagnetic study of the Afyon region, central Turkey
(ELSEVIER SCIENCE BV, 2003)
Following final closure of the Neotethyan Ocean during the late Miocene, deformation in central Turkey has led to crustal thickening and uplift to produce the Anatolian Plateau followed by westward extrusion of terranes ...
Late cenozoic stress evolution along the Karasu Valley, SE Turkey
(ELSEVIER SCIENCE BV, 2004)
This study defines the Mio-Pliocene to present-day stress regime acting at the northeastern comer of the eastern Mediterranean region along the Karasu Valley (i.e., the Amanos Range), taking in the Antakya, Osmaniye and ...
Palaeomagnetic evidence for the Gondwanian origin of the Taurides and rotation of the Isparta Angle, southern Turkey
(WILEY-BLACKWELL, 2002)
The Taurides, the southernmost of the three major tectonic domains that constitute present-day Turkey, were emplaced following consumption of the Tethyan Ocean in Late Mesozoic to mid-Tertiary times. They are generally ...
Paleomagnetic analysis of neotectonic deformation in the Anatolian accretionary collage, Turkey
(Geological Society of America, 2006)
Closure of the Neo-Tethyan Ocean in the Turkish sector of the Alpine-Himalayan orogen by ca. 12 Ma was succeeded by deformation of a domain between the Eurasia plate, presently bounded by the North Anatolian fault, and the ...
Differential neotectonic rotations in Anatolia and the Tauride Arc: Palaeomagnetic investigation of the Erenlerda? Volcanic Complex and Isparta volcanic district, South-central Turkey
(Geological Society of London, 2002)
In the Anatolian sector of the Alpine-Himalayan collisional belt a palaeotectonic phase of terrane accretion has been succeeded by a neotectonic phase of intracontinental deformation as the Afro-Arabian plate has continued ...
Neotectonic deformation linking the east Anatolian and Karataš-Osmaniye intracontinental transform fault zones in the Gulf of ?Iskenderun, southern Turkey, deduced from paleomagnetic study of the Ceyhan-Osmaniye volcanics
(2003)
Left-lateral strike slip along the Dead Sea Fault Zone (DSFZ) between the African and Arabian plates is partitioned into a complex set of motions at its northern extension where Arabia impinges into the Anatolian collage. ...