Relaxation on the Ismetpasa segment of the North Anatolian Fault after the Golcuk Mw = 7.4 and Duzce Mw = 7.2 shocks

The Ismetpasa segment of the North Anatolian Fault (NAF) is a rare place where aseismic fault slip (creep) has been observed. Its creep behaviour has been monitored using different observation methods since the 1950s. The findings obtained from the studies until 1990s showed that the creep rate exponentially decreased before the major shocks in 1999, Golcuk (Mw = 7.4) and Duzce (Mw = 7.2). After these shocks, three GPS periods observation in 2002, 2007 and 2008 were carried out on the geodetic network established around the segment. The evaluations of these observations showed that the creep behaviour relaxed after the major earthquakes. This result demonstrates that the creep behaviour of the Ismetpasa segment might be a warning before future major earthquakes. © 2010 Author(s).

Yazar Kutoglu H.S.
Akcin H.
Gundogdu O.
Gormus K.S.
Koksal E.
Yayın Türü Article
Tek Biçim Adres https://hdl.handle.net/20.500.12628/7373
Tek Biçim Adres 10.5194/nhess-10-2653-2010
Koleksiyonlar Araştırma Çıktıları | WoS | Scopus | TR-Dizin | PubMed | SOBİAD
Scopus İndeksli Yayınlar Koleksiyonu
Dergi Adı Natural Hazards and Earth System Science
Dergi Cilt Bilgisi 10
Dergi Sayısı 12
Sayfalar 2653 - 2657
Yayın Yılı 2010
Eser Adı
[dc.title]
Relaxation on the Ismetpasa segment of the North Anatolian Fault after the Golcuk Mw = 7.4 and Duzce Mw = 7.2 shocks
Yazar
[dc.contributor.author]
Kutoglu H.S.
Yazar
[dc.contributor.author]
Akcin H.
Yazar
[dc.contributor.author]
Gundogdu O.
Yazar
[dc.contributor.author]
Gormus K.S.
Yazar
[dc.contributor.author]
Koksal E.
Yayın Yılı
[dc.date.issued]
2010
Yayın Türü
[dc.type]
article
Özet
[dc.description.abstract]
The Ismetpasa segment of the North Anatolian Fault (NAF) is a rare place where aseismic fault slip (creep) has been observed. Its creep behaviour has been monitored using different observation methods since the 1950s. The findings obtained from the studies until 1990s showed that the creep rate exponentially decreased before the major shocks in 1999, Golcuk (Mw = 7.4) and Duzce (Mw = 7.2). After these shocks, three GPS periods observation in 2002, 2007 and 2008 were carried out on the geodetic network established around the segment. The evaluations of these observations showed that the creep behaviour relaxed after the major earthquakes. This result demonstrates that the creep behaviour of the Ismetpasa segment might be a warning before future major earthquakes. © 2010 Author(s).
Kayıt Giriş Tarihi
[dc.date.accessioned]
2019-12-23
Açık Erişim Tarihi
[dc.date.available]
2019-12-23
Yayın Dili
[dc.language.iso]
eng
Haklar
[dc.rights]
info:eu-repo/semantics/openAccess
ISSN
[dc.identifier.issn]
1561-8633
İlk Sayfa Sayısı
[dc.identifier.startpage]
2653
Son Sayfa Sayısı
[dc.identifier.endpage]
2657
Dergi Adı
[dc.relation.journal]
Natural Hazards and Earth System Science
Dergi Sayısı
[dc.identifier.issue]
12
Dergi Cilt Bilgisi
[dc.identifier.volume]
10
Tek Biçim Adres
[dc.identifier.uri]
https://dx.doi.org/10.5194/nhess-10-2653-2010
Tek Biçim Adres
[dc.identifier.uri]
https://hdl.handle.net/20.500.12628/7373
Görüntülenme Sayısı ( Şehir )
Görüntülenme Sayısı ( Ülke )
Görüntülenme Sayısı ( Zaman Dağılımı )
Görüntülenme
143
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İndirme
1
09.12.2022 tarihinden bu yana
Son Erişim Tarihi
16 Temmuz 2024 23:22
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behaviour segment showed observation earthquakes before Ismetpasa shocks periods carried demonstrates Author(s) future warning result geodetic relaxed observations evaluations around network established different aseismic (creep) observed Anatolian monitored methods findings obtained studies exponentially decreased Golcuk
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