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akaturk Akademik ölçüm

Makale detayı · 2024

Palaeoseismological assessment for a seismic gap located very close to the epicentre of the 30 October 2020 Samos Earthquake (M6.9), western Anatolia, Turkey

Natural Hazards

YÖKSİS OpenAlex Açık erişim · hybrid SJR Q1 JCR Q1 Atıf 14 Üst %10 Yüzdelik 95.5% FWCI 4.45
Yıl
2024
ISSN
0921-030X
Tür
article

Veri kaynağı ayrımı

  • YÖKSİS YÖKSİS makale kaydı
  • OpenAlex OpenAlex zenginleştirmesi (özet, atıf, konular)

Özet

İngilizce (OpenAlex)

Abstract The Tuzla Fault (TF), considered one of the most important seismic sources in İzmir province, is defined as a strike–slip fault with N10E–N60E striking between Gaziemir and Doğanbey districts. A 50-km-long fault consists of three segments which are, from north to south Çatalca, Orhanlı, and Doğanbey segments. Recent studies claim that the part of the TF extending to Kuşadası Bay is also in a kinematic relationship with the Samos Fault that caused an earthquake on 30 October 2020 (Mw = 6.9). In this study, in order to analyse the historical behaviour of the fault, three trench-based palaeoseismology studies across the fault scarp were conducted on three geometric segments of the TF. Palaeoseismology findings show that seven historic/prehistoric earthquakes were generated by TF. According to Oxcal distribution using the Bayesian methods, the time of the events lie between 46.2 ± 6.1 and 1.6 ± 0.3 ka. When the events are compared with the historical earthquakes, the last event is correlated with the earthquakes of 47 AD and/or 177/178 AD on the Doğanbey segment. Moreover, the other events can be attributed to the late Pleistocene–Holocene earthquakes that are prehistorical periods. Our results provide a recurrence interval of an earthquake along the TF to between 0.7 and 4.3 ka for the Holocene period. The elapsed time since the most recent surface faulting earthquake on the TF is 1844 years. It is suggested that it is predicted that TF has the potential to produce destructive earthquakes in the near future, especially in Orhanlı and Çatalca segments which may be considered as a seismic gap.

Konular

  • earthquake and tectonic studies
  • Earthquake Detection and Analysis
  • High-pressure geophysics and materials

Birincil konu earthquake and tectonic studies

Yazarlar

  1. UMUT ÖNCÜ
  2. HASAN SÖZBİLİR
  3. ÇAĞLAR ÖZKAYMAK
  4. MUSTAFA SOFTA
  5. ÖKMEN SÜMER
  6. SEMİH ESKİ
  7. JOEL Q. G. SPENCER
  8. EREN ŞAHİNER ANKARA ÜNİVERSİTESİ
  9. MEHMET YÜKSEL ÇUKUROVA ÜNİVERSİTESİ
  10. NİYAZİ MERİÇ
  11. MUSTAFA TOPAKSU