Palaeoseismological investigations on the Karadere segment, North Anatolian Fault Zone, Turkey

17 Ağustos 1999 İzmit depremi ile Kuzey Anadolu Fayı’nın (KAF) Marmara Bölgesindeki beş segmenti kırılmıştır. Bu segmentlerden en doğudaki Karadere segmentidir. Kırılan diğer segmentler yaklaşık doğu–batı konumlu iken Karadere segmenti hem K65°D doğrultusu ile hem de diğer segmentlerde ölçülen ötelenme değerlerinden daha düşük ötelenme değerleri ile farklılık gösterir. Karadere segmenti üzerinde meydana gelmiş eski depremleri belirleyebilmek amacıyla segmentin orta kesimlerinde iki farklı lokasyonda (Kazimiye ve Karadere lokasyonları) paleosismolojik hendek çalışmaları yapılmıştır. Kazimiye hendeğinde 4.yy’dan sonra 1999 İzmit depremi dahil beş olay tespit edilmiştir. Karbon-14 tarihlendirmesine göre en eski olay M.S. 231–407’den sonra M.S. 420–584’den önce meydana gelmiştir. Bu olay seviyesi M.S. 358 veya M.S. 554 tarihsel depremlerinden birini temsil edebilir. Hendekte belirlenen daha genç üç olay seviyesi ise M.S. 420–584’den sonra 1999 tarihinden önce meydana gelmiştir. Karadere hendeğinde ise 1999 İzmit depremi dahil üç eski olay seviyesi belirlenmiştir. Bu seviyelere göre 1999 depreminden bir önceki olay M.S. 1298–1370’den sonra meydana gelmiştir. Daha yaşlı olan olay seviyesi ise M.S. 1150–1261’den önce meydana gelen bir depremi temsil etmektedir ve Kazimiye hendeğinde izlenen depremlerden biri ile deneştirilebilir. Palaeosismolojik veriler Karadere segmenti üzerinde M.S. 231–407’den sonra 1999 İzmit depremi dahil beş eski depremi işaret etmektedir.

Karadere segmenti üzerinde paleosismolojik araştırmalar, Kuzey Anadolu Fay Zonu, Türkiye

Th e Karadere segment of the North Anatolian Fault (NAF) is the easternmost part that ruptured during the 17 August 1999 İzmit earthquake (Mw 7.4). It has a diff erent orientation, at N65°E to other segments which have a nearly E–W trend, and lesser dextral displacement, with maximum 2.3 m in contrast with 5.2 m in the ruptured neighbouring western segment. Two palaeoseismological trenches, at Kazimiye and Karadere sites, were excavated on the central part of the Karadere segment to determine the timing of past earthquakes. Excavation of the Kazimiye site revealed the occurrence of fi ve past events since the 4th century A.D., including the 1999 İzmit earthquake. Th e oldest event occurred aft er A.D. 231–407 and before A.D. 420–584 based on 14C dating results. Th is event may correspond to either the A.D. 358 earthquake or the A.D. 554 historical earthquake. Th e younger three events predate 1999 and postdate A.D. 420–584. At the Karadere trench site, three past events, including the 1999 İzmit earthquake, were identifi ed. Th e penultimate event was observed on the trench wall and dated to be aft er A.D. 1298–1370. Th e older event is dated as before A.D. 1150–1261, which may correspond to one of the determined events in the Kazimiye trench. In summary, palaeoseismological data provide evidence for at least fi ve large earthquakes on the Karadere segment since A.D. 231–407, including the 1999 İzmit earthquake.

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Turkish Journal of Earth Sciences-Cover
  • ISSN: 1300-0985
  • Yayın Aralığı: Yılda 6 Sayı
  • Yayıncı: TÜBİTAK
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