Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Müge Yazıcı"'
Autor:
İrem Çakır, Cengiz Zabcı, Mehmet Köküm, Hatice Ünal Ercan, Havva Neslihan Kıray, Müge Yazıcı, Mehran Basmenji, Özlem Yağcı, N. Beste Şahinoğlu, Uğur Doğan, Semih Ergintav
The multi-disciplinary studies yield a more complicated picture on seismic cycles, especially with the increasing evidence on creeping, slow slip events, tremors and repeating earthquakes. Recent observations support triggering of large earthquakes e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3638589143f84c4198259b91524a3675
https://doi.org/10.5194/egusphere-egu23-14310
https://doi.org/10.5194/egusphere-egu23-14310
Autor:
Erdem Kırkan, Hüsnü Serdar Akyüz, Mehran Basmenji, Aynur Dikbaş, Cengiz Zabcı, Müge Yazıcı, Mehmet Korhan Erturaç
Publikováno v:
Natural Hazards
The Milas Fault (MF) is a poorly understood active fault located between the Büyük Men- deres graben to the north and the Gökova graben to the south within the Anatolian–Aegean Region, SW Türkiye. This dextral strike-slip fault has a length of
Publikováno v:
Journal of Seismology. 25:255-272
The Ovacik Fault (OF) is one of the internal structures of the Anatolian Block, located close to its eastern boundary. Although it shows a very clear surface trace, there are no instrumentally recorded surface rupturing earthquakes on this fault. Thi
Autor:
Müge Yazıcı, A. M. Celâl Şengör
Publikováno v:
Mediterranean Geoscience Reviews. 2:327-339
The neotectonics of Turkey comprises a time slice since about the end of the Oligocene and has been dominated by the shortening of Eastern Turkey, which created the Turkish–Iranian high plateau, extension in western Turkey, which created the Aegean
Autor:
Erdem KIRKAN, H. Serdar Akyüz, Mehran Basmenji, Aynur Dikbaş, Cengiz Zabcı, Müge Yazıcı, M. Korhan Erturaç
The Milas Fault (MF) is a poorly known active fault located between the Büyük Menderes Graben to the north and the Gökova Graben to the south within the Anatolia-Aegean Region, SW Turkey. This dextral strike-slip fault has a length of 55 km betwee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49f7ab3c730319aef2e68cded0def988
https://doi.org/10.21203/rs.3.rs-1131503/v1
https://doi.org/10.21203/rs.3.rs-1131503/v1
In the complex tectonic setting of the Eastern Mediterranean, the westward motion of the Anatolian Block is accommodated mainly along its boundary faults, the North Anatolian Shear Zone (NASZ) and the East Anatolian Shear Zone (EASZ). Although there
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4efa5600a7facb70edeb8038a3b5f6eb
https://doi.org/10.5194/egusphere-egu2020-843
https://doi.org/10.5194/egusphere-egu2020-843
Anatolia is part of the west-central Alpide plate-boundary zone, particularly where the deformation is characterized by the westward extrusion of this continental block between the Arabian-Eurasian collision in the east and the Hellenic Subduction in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c7e4f143ea7c9fba1faa30dd1019b15
https://doi.org/10.5194/egusphere-egu2020-18856
https://doi.org/10.5194/egusphere-egu2020-18856
Autor:
Marcus Christl, Taylan Sançar, Christof Vockenhuber, Susan Ivy-Ochs, Cengiz Zabcı, H. Serdar Akyüz, Müge Yazıcı, Ayten Öztüfekçi Önal, Serdar Yeşilyurt, Volkan Karabacak, Naki Akçar
Controversy remains over when present-day configuration of the Anatolia boundary faults came into existence, and the issue of what are the driving forces of the Anatolian westward motion. The NW-striking dextral and NE-striking sinistral second-order
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6ba806e8a67c95ee80becfdc12af058b
https://aperta.ulakbim.gov.tr/record/4483
https://aperta.ulakbim.gov.tr/record/4483
Publikováno v:
Journal of Nanotechnology, Vol 2012 (2012)
Whole bacterial cell characterization is critically important for fast bacterial identification. Surface-enhanced Raman scattering (SERS) is proven to be powerful technique to serve such a goal. In this study, the characterization of whole bacterial
Externí odkaz:
https://doaj.org/article/6486d4e4594a4bf49a9c714449f1d8fe
The sinistral Malatya-Ovacik Fault Zone (MOFZ) is one of the outstanding intraplate deformation belts within Anatolia. The 165-km-long, NE–SW-striking Malatya Fault (MF), which constitutes the southern section of the MOFZ, is separated into five se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::320536d9d63ffe65c68c080a5939c372
https://hdl.handle.net/20.500.12406/201
https://hdl.handle.net/20.500.12406/201