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THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA

Year 2013, Volume: 147 Issue: 147, 1 - 17, 01.12.2013

Abstract

The North Anatolian Fault (NAF), which is an intra-continental transform fault, is divided into two branches as Northern and Southern branches in Marmara Region. The southern branch which separates from each other by rightward stepovers between Bandırma and Dokurcun valley is formed by three main fault segments as Geyve, İznik and Gemlik from East to West. The length of fault segments ranges between 40 and 57 km and GPS data in Southern branch propose a 5 mm/year slip rate. Two surface faulting events were observed during paleoseismological excavations which had been carried out on 40 km long Gemlik segment and these can be correlated with earthquakes that occurred in 1857 and 1419. The recurrence interval between the last two earthquakes in Gemlik Fault is 438 years. Findings indicate that Gemlik fault was also included into surface faulting of the earthquake in 1419 which its presence is known in İznik fault. At least 95 km long multi-segment surface faulting developed in this earthquake. Based on 5 mm/years slip rate, the cumulative offset amount slip rate of NAF was approximately estimated as 3 meters in 595 years in region between İznik Lake and Dokurcun Valley. Accordingly; it can be stated that the southern branch of the North Anatolian Fault has a potential to trigger a large earthquake as well as the Northern branch

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Year 2013, Volume: 147 Issue: 147, 1 - 17, 01.12.2013

Abstract


References

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There are 83 citations in total.

Details

Primary Language English
Subjects Engineering
Journal Section Articles
Authors

Selim Özalp This is me

Ömer Emre This is me

Ahmet Doğan This is me

Publication Date December 1, 2013
Published in Issue Year 2013 Volume: 147 Issue: 147

Cite

APA Özalp, S., Emre, Ö., & Doğan, A. (2013). THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA. Bulletin of the Mineral Research and Exploration, 147(147), 1-17.
AMA Özalp S, Emre Ö, Doğan A. THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA. Bull.Min.Res.Exp. December 2013;147(147):1-17.
Chicago Özalp, Selim, Ömer Emre, and Ahmet Doğan. “THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA”. Bulletin of the Mineral Research and Exploration 147, no. 147 (December 2013): 1-17.
EndNote Özalp S, Emre Ö, Doğan A (December 1, 2013) THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA. Bulletin of the Mineral Research and Exploration 147 147 1–17.
IEEE S. Özalp, Ö. Emre, and A. Doğan, “THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA”, Bull.Min.Res.Exp., vol. 147, no. 147, pp. 1–17, 2013.
ISNAD Özalp, Selim et al. “THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA”. Bulletin of the Mineral Research and Exploration 147/147 (December 2013), 1-17.
JAMA Özalp S, Emre Ö, Doğan A. THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA. Bull.Min.Res.Exp. 2013;147:1–17.
MLA Özalp, Selim et al. “THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA”. Bulletin of the Mineral Research and Exploration, vol. 147, no. 147, 2013, pp. 1-17.
Vancouver Özalp S, Emre Ö, Doğan A. THE SEGMENT STRUCTURE OF SOUTHERN BRANCH OF THE NORTH ANATOLIAN FAULT AND PALEOSEISMOLOGICAL BEHAVIOUR OF THE GEMLİK FAULT, NW ANATOLIA. Bull.Min.Res.Exp. 2013;147(147):1-17.

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