Şarköy-Mürefte 1912 Earthquake's Tsunami, extension of the associated faulting in the Marmara Sea, Turkey

Y. Altınok; B. Alpar; C. Yaltırak

doi:10.1023/A:1024581022222

Şarköy-Mürefte 1912 Earthquake's Tsunami, extension of the associated faulting in the Marmara Sea, Turkey

Y. Altınok^*, B. Alpar, C. Yaltırak

^*Bu çalışma için yazışmadan sorumlu yazar

Jeoloji Mühendisliği Bölümü

Istanbul University

Araştırma sonucu: Dergiye katkı › Makale › bilirkişi

46 Atıf (Scopus)

Özet

The historical tsunamis in the Marmara Sea were mainly caused by earthquakes and needed to be documented. Following 1999 Izmit earthquake occurred at the Eastern Marmara region, a complete inventory of active faults in the Marmara Sea region became much more stressed. To the west, the latest event is 09.08.1912 Sarköy-Mürefte Earthquake. It occured on the active Ganos Fault zone and was one of the largest earthquakes in the Balkans. The eastern termination of the associated faulting is in the deep West Marmara Trough, westernmost of the successive basins forming the Marmara Sea. On the basis of recent multibeam bathymetry and seismic reflection data, estimated total length of the surface rupture is about 56 km. The historical data reviewed from library and archive documents, geological field surveys and offshore geophysical investigation have shown that the 1912 earthquake produced a tsunami. In addition a seabed dislocation, the source of 1912 tsunami can also be assigned to the sediment slumps appearing in the form of echelon landslide prisms along the southern slopes of the West Marmara Trough.

Orijinal dil	İngilizce
Sayfa (başlangıç-bitiş)	329-346
Sayfa sayısı	18
Dergi	Journal of Seismology
Hacim	7
Basın numarası	3
DOI'lar	https://doi.org/10.1023/A:1024581022222
Yayın durumu	Yayınlandı - Tem 2003

Finansman

This paper is an extended version of the note presented at the NATO ARW, Underwater Ground Failures on Tsunami Generation, Modeling, Risk and Mitigation, held in Istanbul in 23–26 May 2001. This work has been partially supported by the Executive Secretariat of the Research Fund of the Istanbul University (B-991/31052001; B-999/31052001; O-1131/09112001). Authors thank to the Turkish Republic Prime Ministry, General Directorate of the State Archives, Istanbul Library, Istanbul Atatürk Library and Hydrographic Department of the Turkish Navy. We also thank Dr Sinan Öngen and Ms. Esra Keskinkilic for their kind helps.

Finansörler	Finansör numarası
Istanbul Üniversitesi	B-999/31052001, O-1131/09112001, B-991/31052001

Belgeye Erişim

10.1023/A:1024581022222

Diğer Dosyalar ve Linkler

Link to publication in Scopus

Alıntı Yap

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title = "{\c S}ark{\"o}y-M{\"u}refte 1912 Earthquake's Tsunami, extension of the associated faulting in the Marmara Sea, Turkey",

abstract = "The historical tsunamis in the Marmara Sea were mainly caused by earthquakes and needed to be documented. Following 1999 Izmit earthquake occurred at the Eastern Marmara region, a complete inventory of active faults in the Marmara Sea region became much more stressed. To the west, the latest event is 09.08.1912 Sark{\"o}y-M{\"u}refte Earthquake. It occured on the active Ganos Fault zone and was one of the largest earthquakes in the Balkans. The eastern termination of the associated faulting is in the deep West Marmara Trough, westernmost of the successive basins forming the Marmara Sea. On the basis of recent multibeam bathymetry and seismic reflection data, estimated total length of the surface rupture is about 56 km. The historical data reviewed from library and archive documents, geological field surveys and offshore geophysical investigation have shown that the 1912 earthquake produced a tsunami. In addition a seabed dislocation, the source of 1912 tsunami can also be assigned to the sediment slumps appearing in the form of echelon landslide prisms along the southern slopes of the West Marmara Trough.",

keywords = "Bathymetry, Marmara Sea, North Anatolian fault, Seismic reflection, Slumping, Tsunami, Underwater failures",

author = "Y. Altınok and B. Alpar and C. Yaltırak",

year = "2003",

month = jul,

doi = "10.1023/A:1024581022222",

language = "English",

volume = "7",

pages = "329--346",

journal = "Journal of Seismology",

issn = "1383-4649",

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T1 - Şarköy-Mürefte 1912 Earthquake's Tsunami, extension of the associated faulting in the Marmara Sea, Turkey

AU - Altınok, Y.

AU - Alpar, B.

AU - Yaltırak, C.

PY - 2003/7

Y1 - 2003/7

N2 - The historical tsunamis in the Marmara Sea were mainly caused by earthquakes and needed to be documented. Following 1999 Izmit earthquake occurred at the Eastern Marmara region, a complete inventory of active faults in the Marmara Sea region became much more stressed. To the west, the latest event is 09.08.1912 Sarköy-Mürefte Earthquake. It occured on the active Ganos Fault zone and was one of the largest earthquakes in the Balkans. The eastern termination of the associated faulting is in the deep West Marmara Trough, westernmost of the successive basins forming the Marmara Sea. On the basis of recent multibeam bathymetry and seismic reflection data, estimated total length of the surface rupture is about 56 km. The historical data reviewed from library and archive documents, geological field surveys and offshore geophysical investigation have shown that the 1912 earthquake produced a tsunami. In addition a seabed dislocation, the source of 1912 tsunami can also be assigned to the sediment slumps appearing in the form of echelon landslide prisms along the southern slopes of the West Marmara Trough.

AB - The historical tsunamis in the Marmara Sea were mainly caused by earthquakes and needed to be documented. Following 1999 Izmit earthquake occurred at the Eastern Marmara region, a complete inventory of active faults in the Marmara Sea region became much more stressed. To the west, the latest event is 09.08.1912 Sarköy-Mürefte Earthquake. It occured on the active Ganos Fault zone and was one of the largest earthquakes in the Balkans. The eastern termination of the associated faulting is in the deep West Marmara Trough, westernmost of the successive basins forming the Marmara Sea. On the basis of recent multibeam bathymetry and seismic reflection data, estimated total length of the surface rupture is about 56 km. The historical data reviewed from library and archive documents, geological field surveys and offshore geophysical investigation have shown that the 1912 earthquake produced a tsunami. In addition a seabed dislocation, the source of 1912 tsunami can also be assigned to the sediment slumps appearing in the form of echelon landslide prisms along the southern slopes of the West Marmara Trough.

KW - Bathymetry

KW - Marmara Sea

KW - North Anatolian fault

KW - Seismic reflection

KW - Slumping

KW - Tsunami

KW - Underwater failures

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DO - 10.1023/A:1024581022222

M3 - Article

AN - SCOPUS:0041852772

SN - 1383-4649

VL - 7

SP - 329

EP - 346

JO - Journal of Seismology

JF - Journal of Seismology

IS - 3

ER -

Şarköy-Mürefte 1912 Earthquake's Tsunami, extension of the associated faulting in the Marmara Sea, Turkey

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