North Anatolian Fault NAF Passive Seismic Experiment Continental Lithospheric Deformation along a Major Strike Slip Fault central Turkey

Date

2009-09-10

Author

Özacar, Atilla Arda
Tok, Hande
Gans, Christine R.
Zandt, George
Beck, Susan L.
Warren, Linda M.
TAYMAZ, TUNCAY

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URI

https://hdl.handle.net/11511/94722

Conference Name

International Symposium on Historical Earthquakes and Conservation of Monuments and Sites in the Eastern Mediterranean Region

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Department of Geological Engineering, Conference / Seminar

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North Anatolian Fault Passive Seismic Experiment Receiver functions along a major strike slip fault Özacar, Atilla Arda; Zandt, George; Beck, Susan L. (2006-12-11)
SOUTHERN MENDERES MASSIF - AN INCIPIENT METAMORPHIC CORE COMPLEX IN WESTERN ANATOLIA, TURKEY Bozkurt, Erdin (Geological Society of London, 1994-03-01) In the southern sector of the Menderes Massif, north of Selimiye (Milas) augen gneisses interpreted as a deformed peraluminous granite have been dynamothermally metamorphosed and are surrounded by and intrude a regionally metamorphosed Palaeozoic 'envelope'. The granitic rocks exhibit a moderately-dipping mylonitic foliation and NNE-SSW- trending mineral elongation lineation. The progressive deformation of the granitic rocks produces a structural sequence typical of an extensional shear zone marked, from bo...
Central Anatolian Seismic Network Initial Analysis of the Seismicity and Earth Structure Özacar, Atilla Arda; Delph, Jonathan; Beck, Susan L; Sandvol, Eric; Türkelli, Niyazi; Kalafat, Doğan; Kahraman, Metin; Teoman, Uğur (2015-04-12)
Eastern Pontides Volcanism and Related Ore Deposits Excursion Guide Çamur, Mehmet Zeki (1994-09-01)
Eastern Termination of the Subducting African Lithosphere Beneath Anatolia Imaged by Teleseismic P wave Tomography Biryol, C. Berk; Zandt, George; Beck, Susan L.; Özacar, Atilla Arda; Schmandt, Brandon (2009-12-14) A variety of complex tectonic processes are active in Anatolia. Collision related plateau formation dominates the present lithospheric deformation toward the east and slab roll-back related back-arc extension takes place toward the west. The two zones are connected at the northern part of the region by strike-slip faulting along the right-lateral North Anatolian Fault. Recent seismological studies show that the Eastern Anatolian Plateau (EAP) is supported by hot asthenosphereric material that was emplaced b...

Citation Formats

A. A. Özacar et al., “North Anatolian Fault NAF Passive Seismic Experiment Continental Lithospheric Deformation along a Major Strike Slip Fault central Turkey,” presented at the International Symposium on Historical Earthquakes and Conservation of Monuments and Sites in the Eastern Mediterranean Region, İstanbul, Türkiye, 2009, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/94722.