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pro vyhledávání: '"Figen Eskikoy"'
On November 23, 2022 an Mw6.0 earthquake struck northwest Turkey. The location of this earthquake is along the boundary of the northeast striking Karadere and east striking Düzce segments of the North Anatolian Fault. Remarkably the area had already
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df30bb17913784163e5bd3a38022b0d6
https://doi.org/10.5194/egusphere-egu23-9062
https://doi.org/10.5194/egusphere-egu23-9062
Publikováno v:
Geophysical Journal International. 224:377-388
SUMMARYThe unbroken section of the North Anatolian Fault beneath the Sea of Marmara is a major source of seismic hazard for the city of İstanbul. The northern and currently the most active branch, the Main Marmara Fault (MMF), is segmented within a
Autor:
Seda Özarpacı, Michael Floyd, Sezim Ezgi Güvercin, Semih Ergintav, Uğur Doğan, A. Ozgun Konca, Alpay Özdemir, Hayrullah Karabulut, Figen Eskikoy
Publikováno v:
Journal of Geophysical Research: Solid Earth. 126
Autor:
Seda Özarpacı, Ali Ozgun Konca, M. Hilmi Erkoç, Semih Ergintav, Alpay Özdemir, İlay Farimaz, Uğur Doğan, Figen Eskikoy, Efe T. Ayruk, Hannes Vasyura-Bathke
On 2020 October 30, an Mw6.9 earthquake struck offshore Samos Island. Severe structural damages were observed in Greek Islands and city of Izmir (Turkey). 114 people lost their lives and more than a thousand people were injured in Turkey. The earthqu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bc00a3ec20ba8331fd0237284555bd30
https://doi.org/10.5194/egusphere-egu21-14970
https://doi.org/10.5194/egusphere-egu21-14970
Autor:
Figen Eskikoy, Efe T. Ayruk, Alpay Özdemir, Muharrem Hilmi Erkoç, Uğur Doğan, İlay Farimaz, Seda Özarpacı, Semih Ergintav
The Samos-Izmir Earthquake (Mw=6.9) of October 30, 2020 is among the strongest earthquakes that occurred in recent years throughout the Eastern Aegean. The epicenter of this earthquake was 14 km away from Samos Island and 25 km away from Gümüldür-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ee0d123f54ae927f6929ce527776bcc
https://doi.org/10.5194/egusphere-egu21-4767
https://doi.org/10.5194/egusphere-egu21-4767
Autor:
Hannes Vasyura-Bathke, Marius Isken, Ziyadin Cakir, Ali Ozgun Konca, Semih Ergintav, Figen Eskikoy, Hayrullah Karabulut
Southwestern Anatolia is part of a N-S extensional regime mainly driven by rollback along the Hellenic subduction zone beneath the Aegean Sea. This seismically active area is controlled primarily by normal fault systems. The fault structures in the r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc2240cedd32381b342c6936d1fb9b2a
https://doi.org/10.5194/egusphere-egu2020-1068
https://doi.org/10.5194/egusphere-egu2020-1068
The North Anatolian Fault (NAF) is a 1600 km dextral transform fault accommodating the motion between Anatolia and Eurasia Plates. The segments beneath the Marmara Sea, are the only part of the NAF that did not break since the 20thcentury. Recent stu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1236d02937e36c116e9992575b8261f
https://doi.org/10.5194/egusphere-egu2020-8438
https://doi.org/10.5194/egusphere-egu2020-8438