Browsing by Author "Tatar O."
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Differential neotectonic rotations in Anatolia and the Tauride Arc: Palaeomagnetic investigation of the Erenlerda? Volcanic Complex and Isparta volcanic district, South-central Turkey
Tatar O.; Gürsoy H.; Piper J.D.A. (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 in the transition zone between the Dead Sea Transform and the East Anatolian Fault Zone, Southern Turkey: A palaeomagnetic study of the Karasu Rift Volcanism
Tatar O.; Piper J.D.A.; Gürsoy H.; Heimann A.; Koçbulut F. (2004)In southern Turkey ongoing differential impingement of Arabia into the weak Anatolian collisional collage resulting from subduction of the Neotethyan Ocean has produced one of the most complex crustal interactions along ... -
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
Gürsoy H.; Tatar O.; Piper J.D.A.; Heimann A.; Mesci L. (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. ... -
Palaeomagnetic study of crustal deformation across an intracontinental transform: The North Anatolian Fault Zone in Northern Turkey
Piper J.D.A.; Moore J.M.; Tatar O.; Gursoy H.; Park R.G. (1996)Eocene volcanic rocks spanning the North Anatolian Fault Zone in north central Turkey have a common reversed polarity and appear to record a short term volcanic episode useful for identifying subsequent tectonic rotations. ... -
Palaeomagnetic study of the Erciyes sector of the Ecemis Fault Zone: Neotectonic deformation in the southeastern part of the Anatolian Block
Tatar O.; Piper J.D.A.; Gürsoy H. (2000)In the Turkish sector of the Afro-Eurasian collision zone, continuing northward motion of the Arabian promontory is extruding the Anatolian region to the west. Although the East Anatolian Fault Zone (EAFZ) is recognized ... -
Paleomagnetic analysis of neotectonic deformation in the Anatolian accretionary collage, Turkey
Piper J.D.A.; Tatar O.; Gursoy H.; Koçbulut F.; Mesci B.L. (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 ... -
Regional significance of neotectonic counterclockwise rotation in central turkey
Tatar O.; Piper J.D.A.; Gürsoy H.; Temiz H. (1996)Counterclockwise rotation is a characteristic feature of the results of most paleomagnetic studies of the Pontides and Anatolides of central Turkey, applicable to regions both north and south of the North Anatolian fault ...