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Full-Text Articles in Physical Sciences and Mathematics
Seismic A And B-Values And Crustal Parameters Of Samos Island-Aegean Sea, Lesvosisland-Karaburun, Kos Island-Gökova Bay Earthquakes, Oya Pamukçu, Fi̇kret Doğru, Ayça Çirmik, Düzgün Göneş
Seismic A And B-Values And Crustal Parameters Of Samos Island-Aegean Sea, Lesvosisland-Karaburun, Kos Island-Gökova Bay Earthquakes, Oya Pamukçu, Fi̇kret Doğru, Ayça Çirmik, Düzgün Göneş
Turkish Journal of Earth Sciences
In recent years, seismicity has increased considerably in the Aegean Sea region and there have been earthquakes in which people lost their lives. The major earthquakes, Kos Island-Gökova Bay (Mw = 6.6), Lesvos Island-Karaburun (İzmir) (Mw = 6.2) and Samos Island-Aegean Sea (Mw = 6.9) occurred in the Aegean Sea and affected Aegean region strongly. Within the scope of this study, the seismic b-value of these major earthquakes was calculated in order to perform earthquake statistical analysis. Seismic a and b-values within the first 24 h and 14 days after the mainshock determination of Kos Island-Gökova Bay, Lesvos Island-Karaburun (İzmir) …
Gps Derived Finite Source Mechanism Of The 30 October 2020 Samos Earthquake, Mw =6.9, In The Aegean Extensional Region, Bahadir Aktuğ, İbrahi̇m Ti̇ryaki̇oğlu, Hasan Sözbi̇li̇r, Haluk Özener, Çağlar Özkaymak, Cemal Özer Yi̇ği̇t, Hali̇l İbrahi̇m Solak, Eda Esma Eyübagi̇l, Bengi̇su Geli̇n, Orhan Tatar, Mustafa Softa
Gps Derived Finite Source Mechanism Of The 30 October 2020 Samos Earthquake, Mw =6.9, In The Aegean Extensional Region, Bahadir Aktuğ, İbrahi̇m Ti̇ryaki̇oğlu, Hasan Sözbi̇li̇r, Haluk Özener, Çağlar Özkaymak, Cemal Özer Yi̇ği̇t, Hali̇l İbrahi̇m Solak, Eda Esma Eyübagi̇l, Bengi̇su Geli̇n, Orhan Tatar, Mustafa Softa
Turkish Journal of Earth Sciences
A submarine area close to the Turkish and Greek border between the cities of Samos-Greece and Seferihisar-Turkey has been shaked on October 30, 2020 by a Mw= 6.9 earthquake. In this study, the finite source mechanism of the Samos earthquake was investigated using geodetic methods and the coseismic behavior of the earthquake was modeled. The observed coseismic displacements at 62 sites were inverted for the fault geometry and the slips. The mainshock did not generate an on-land surface rupture. However, the uniform slip modeling shows a finite source of 43.1 km long and 16 km wide rupture, which slips 1.42 …