Historical earthquake activity of the northern part of the Dead Sea Fault Zone, southern Turkey

H. Serdar Akyuz; Erhan Altunel; Volkan Karabacak; C. Caglar Yalciner

doi:10.1016/j.tecto.2006.08.005

Historical earthquake activity of the northern part of the Dead Sea Fault Zone, southern Turkey

H. Serdar Akyuz^*, Erhan Altunel, Volkan Karabacak, C. Caglar Yalciner

^*Bu çalışma için yazışmadan sorumlu yazar

Jeoloji Mühendisliği Bölümü

Osmangazi University

Araştırma sonucu: ???type-name??? › Makale › bilirkişi

67 Atıf (Scopus)

Özet

The northern part of the Dead Sea Fault Zone is one of the major active neotectonic structures of Turkey. The main trace of the fault zone (called Haci{dotless}paşa fault) is mapped in detail in Turkey on the basis of morphological and geological evidence such as offset creeks, fault surfaces, shutter ridges and linear escarpments. Three trenches were opened on the investigated part of the fault zone. Trench studies provided evidence for 3 historical earthquakes and comparing trench data with historical earthquake records showed that these earthquakes occurred in 859 AD, 1408 and 1872. Field evidence, palaeoseismological studies and historical earthquake records indicate that the Haci{dotless}paşa fault takes the significant amount of slip in the northern part of the Dead Sea Fault Zone in Turkey. On the basis of palaeoseismological evidence, it is suggested that the recurrence interval for surface faulting event is 506 ± 42 years on the Haci{dotless}paşa fault.

Orijinal dil	İngilizce
Sayfa (başlangıç-bitiş)	281-293
Sayfa sayısı	13
Dergi	Tectonophysics
Hacim	426
Basın numarası	3-4
DOI'lar	https://doi.org/10.1016/j.tecto.2006.08.005
Yayın durumu	Yayınlandı - 15 Kas 2006

Finansman

This research is supported by the ongoing European Commission project (ICA-CT-2002-10024, Co-ordinated by Mustapha Meghraoui), Eskişehir Osmangazi University Research Foundation (200415001) and TUBITAK (105Y021). Altan Devrim, Umut Akyüz and Önder Yönlü assisted in the field, and Aynur Dikbaş in office works. We are grateful to Mr. Abdüssemii Erkan (Mayor of Hacıpaşa Town) for his logistic support. Our special thanks go to Central and local Military Authorities for giving permission to work in the area. Dating analyses were carried out in the laboratory of University of Kiel running by Pieter Grootes. We are grateful for the helpful comments and constructive reviews by S. Marco and an anonymous reviewer, which improved our manuscript.

Finansörler	Finansör numarası
Eskişehir Osmangazi University Research Foundation	200415001
TUBITAK	105Y021

BM SKH

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Belgeye Erişim

10.1016/j.tecto.2006.08.005

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Link to publication in Scopus

Alıntı Yap

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title = "Historical earthquake activity of the northern part of the Dead Sea Fault Zone, southern Turkey",

abstract = "The northern part of the Dead Sea Fault Zone is one of the major active neotectonic structures of Turkey. The main trace of the fault zone (called Haci{dotless}pa{\c s}a fault) is mapped in detail in Turkey on the basis of morphological and geological evidence such as offset creeks, fault surfaces, shutter ridges and linear escarpments. Three trenches were opened on the investigated part of the fault zone. Trench studies provided evidence for 3 historical earthquakes and comparing trench data with historical earthquake records showed that these earthquakes occurred in 859 AD, 1408 and 1872. Field evidence, palaeoseismological studies and historical earthquake records indicate that the Haci{dotless}pa{\c s}a fault takes the significant amount of slip in the northern part of the Dead Sea Fault Zone in Turkey. On the basis of palaeoseismological evidence, it is suggested that the recurrence interval for surface faulting event is 506 ± 42 years on the Haci{dotless}pa{\c s}a fault.",

keywords = "Dead Sea Fault Zone, Historical earthquake, Palaeoseismology, Southern Turkey, Trench",

author = "Akyuz, {H. Serdar} and Erhan Altunel and Volkan Karabacak and Yalciner, {C. Caglar}",

year = "2006",

month = nov,

day = "15",

doi = "10.1016/j.tecto.2006.08.005",

language = "English",

volume = "426",

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journal = "Tectonophysics",

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T1 - Historical earthquake activity of the northern part of the Dead Sea Fault Zone, southern Turkey

AU - Akyuz, H. Serdar

AU - Altunel, Erhan

AU - Karabacak, Volkan

AU - Yalciner, C. Caglar

PY - 2006/11/15

Y1 - 2006/11/15

N2 - The northern part of the Dead Sea Fault Zone is one of the major active neotectonic structures of Turkey. The main trace of the fault zone (called Haci{dotless}paşa fault) is mapped in detail in Turkey on the basis of morphological and geological evidence such as offset creeks, fault surfaces, shutter ridges and linear escarpments. Three trenches were opened on the investigated part of the fault zone. Trench studies provided evidence for 3 historical earthquakes and comparing trench data with historical earthquake records showed that these earthquakes occurred in 859 AD, 1408 and 1872. Field evidence, palaeoseismological studies and historical earthquake records indicate that the Haci{dotless}paşa fault takes the significant amount of slip in the northern part of the Dead Sea Fault Zone in Turkey. On the basis of palaeoseismological evidence, it is suggested that the recurrence interval for surface faulting event is 506 ± 42 years on the Haci{dotless}paşa fault.

AB - The northern part of the Dead Sea Fault Zone is one of the major active neotectonic structures of Turkey. The main trace of the fault zone (called Haci{dotless}paşa fault) is mapped in detail in Turkey on the basis of morphological and geological evidence such as offset creeks, fault surfaces, shutter ridges and linear escarpments. Three trenches were opened on the investigated part of the fault zone. Trench studies provided evidence for 3 historical earthquakes and comparing trench data with historical earthquake records showed that these earthquakes occurred in 859 AD, 1408 and 1872. Field evidence, palaeoseismological studies and historical earthquake records indicate that the Haci{dotless}paşa fault takes the significant amount of slip in the northern part of the Dead Sea Fault Zone in Turkey. On the basis of palaeoseismological evidence, it is suggested that the recurrence interval for surface faulting event is 506 ± 42 years on the Haci{dotless}paşa fault.

KW - Dead Sea Fault Zone

KW - Historical earthquake

KW - Palaeoseismology

KW - Southern Turkey

KW - Trench

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U2 - 10.1016/j.tecto.2006.08.005

DO - 10.1016/j.tecto.2006.08.005

M3 - Article

AN - SCOPUS:33749986994

SN - 0040-1951

VL - 426

SP - 281

EP - 293

JO - Tectonophysics

JF - Tectonophysics

IS - 3-4

ER -

Historical earthquake activity of the northern part of the Dead Sea Fault Zone, southern Turkey

Özet

Finansman

BM SKH

Belgeye Erişim

Diğer Dosyalar ve Linkler

Parmak izi

Alıntı Yap