Gezgin, Cemil; Solak, Halil Ibrahim; Tiryakioğlu, İbrahim; Ozener, Haluk; Aktug, Bahadir; Yalvac, Sefa; Eyübagil, Eda Esma; Yigit, Cemal Ozer; Demirelli, Ertuğrul; Çakanşimşek, Ece Bengünaz

Solak, H., Tiryakioğlu, İ., Yalvaç, S., Yiğit, C.Ö., Aktuğ, B., Özener, H., Dönmez, E., Demirelli, E., Eyübagil, E.E., Çakanşimşek, E.B., Gezgin, C., Şahiner, F., 2024. 30 Ekim 2020 Mw:6.9 Sisam Depremi Sonrası İzmir ve Çevresinde Postsismik Deformasyonların İzlenmesi, Afyon Kocatepe Üniversitesi, Fen ve Mühendislik Bilimleri Dergisi, 24 (6): 1442-1455. https://doi.org/10.35414/akufemubid.1465489 Yukarıda künye bilgileri verilen makale için yazar tarafından düzeltme talebinde bulunulmuştur. Makalenin kaynakça bölümünde yer alan “Çırmık, A., Pamukçu, O. and Gönenç, T., 2017. The Stress/Strain Analysis of Kinematic Structure at Gülbahce Fault and Uzunkuyu Intrusive (İzmir, Turkey). Pure and Applied Geophysics, 174, 1425- 1440. https://doi.org/10.1007/s00024-017-1474-5” kaynağının sehven hatalı olarak yazıldığı makale yayınından sonra tespit edilmiştir. Yazarın yazılı talebine istinaden ilgili kaynak aşağıda belirtilen şekliyle düzeltilmiştir. Okuyucuların ve kullanıcıların bilgisine sunarız.

Gezgin, Cemil; Solak, Halil Ibrahim; Tiryakioğlu, İbrahim; Ozener, Haluk; Aktug, Bahadir; Yalvac, Sefa; Eyübagil, Eda Esma; Yigit, Cemal Ozer; Demirelli, Ertuğrul; Çakanşimşek, Ece Bengünaz

A devastating (Mw: 6.9) earthquake occurred in the north of Samos island on October 30, 2020. This earthquake caused loss of life and property in Izmir city center and some districts. After the earthquake, studies conducted in Izmir and its south showed that there was a horizontal displacement of 4-14 cm in Izmir and its south, the largest of which was in Seferihisar. In this region, there are many active faults with the potential to produce earthquakes between Mw:6.1 and Mw:6.9. A 27-site GNSS network has been established to monitor the postseismic deformation in this region since an earthquake can affect the earthquakes that may be caused by other surrounding faults. 4 GNSS campaign measurements were conducted over 6-month periods between 2020 and 2022 in this network. Eurasian fixed velocities of all sites were obtained using GNSS data. The results obtained show that the differences between both the current velocities and the pre-earthquake velocities in the network have reached 6 mm, and accordingly, the postseismic deformation continues in the region.