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Extensional Neotectonic Regime through the NE Edge of the Outer Isparta Angle, SW Turkey: New Field and Seismic Data
Date
2003-05-01
Author
Koçyiğit, Ali
Özacar, Atilla Arda
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http://journals.tubitak.gov.tr/earth/issues/yer-03-12-1/yer-12-1-5-0301-4.pdf
https://hdl.handle.net/11511/81989
Journal
Turkish Journal Of Earth Sciences
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Extensional neotectonic regime through the NE edge of the outer Isparta Angle, SW Turkey: New field and seismic data
Özacar, Atilla Arda (2003-01-01)
The Akşehir-Afyon Graben (AAG) is a 4-20-km-wide, 130-km-long NW-trending depression that separates central Anatolia in the NE and the Isparta Angle (IA) in the SW. Its southwestern margin-bounding fault determines the northeast edge of the outer IA that was previously interpreted as a compressional neotectonic structure, whereas our field evidence and recent seismic data substantiated that it is an oblique-slip normal fault characterising an extensional neotectonic regime. The AAG has an episodic and asymm...
Extensional tectonics of SW Anatolia in relation to slab edge processes in the Eastern Mediterranean
Kaymakcı, Nuretdin; Özkaptan, Murat; Özacar, Atilla Arda; Uzel, Bora; Gülyüz, Erhan; Sözbilir, Hasan (null; 2017-12-14)
The tectonics of SW Anatolia is expressed in terms of emplacement of Lycian Nappes during the Eocene to Middle Miocene and synconvergent extension as part of the Aegean-West Anatolian extensional tectonic regime. Recent studies identified that there is a tear in the northwards subducting African Oceanic lithosphere along the Pliny-Strabo Trenches (PST). Such tears are coined as Subduction Transform-Edge Propagator (STEP) faults developed high angle to trenches. Hypothetically, the evolution of a STEP fault ...
Erosional truncation of uppermost Permian shallow-marine carbonates and implications for Permian-Triassic boundary events: Reply
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Neotectonics and seismicity of eastern simav graben, Kütahya – Turkey
Kaplan, Mustafa; Koçyiğit, Ali; Department of Geological Engineering (2014)
The Simav graben is an about 1-9 km wide, 50 km long and approximately WNW-trending active depression. It is located along the western section of a seismogenic belt with a depth of 10-15 km. It is the 10-30 km wide and approximately 500 km long active fault system, namely the Akşehir-Simav fault system. The Simav graben was developed on the northern Menderes Massif under the control of active faults comprising the Simav section of the Akşehir-Simav fault system. The Simav and Akdere grabens include two diff...
Erosional truncation of uppermost Permian shallow-marine carbonates and implications for Permian-Triassic boundary events
Payne, Jonathan L.; Lehrmann, Daniel J.; Follett, David; Seibel, Margaret; Kump, Lee R.; Riccardi, Anthony; Altıner, Demir; Sano, Hiroyoshi; Wei, Jiayong (Geological Society of America, 2007-07-01)
On shallow-marine carbonate buildups in south China, Turkey, and Japan, uppermost Permian skeletal limestones are truncated by an erosional surface that exhibits as much as 10 cm of topography, including overhanging relief. Sedimentary facies, microfabrics, carbon isotopes, and cements together suggest that erosion occurred in a submarine setting. Moreover, biostratigraphic data from south China demonstrate that the surface postdates the uppermost Permian sequence boundary at the global stratotype section a...
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A. Koçyiğit and A. A. Özacar, “Extensional Neotectonic Regime through the NE Edge of the Outer Isparta Angle, SW Turkey: New Field and Seismic Data,”
Turkish Journal Of Earth Sciences
, pp. 67–90, 2003, Accessed: 00, 2021. [Online]. Available: http://journals.tubitak.gov.tr/earth/issues/yer-03-12-1/yer-12-1-5-0301-4.pdf.