Morphotectonics of the sea of marmara: Basins and highs on the north anatolian continental transform plate boundary

M. Namık Çağatay; Gülsen Uçarkuş

doi:10.1016/B978-0-12-812064-4.00016-5

Morphotectonics of the sea of marmara: Basins and highs on the north anatolian continental transform plate boundary

M. Namık Çağatay
, Gülsen Uçarkuş

Jeoloji Mühendisliği Bölümü

Istanbul Technical University

Araştırma sonucu: Kitap/Rapor/Konferans Bildirisinde Bölüm › Bölüm › bilirkişi

18 Atıf (Scopus)

Özet

The Sea of Marmara is located in the North Anatolian Fault (NAF), a major continental transform plate boundary between the Eurasian and Anatolian-Aegean plates. The area is also under the influence of the N-S extensional Aegean regime. The 100 km-wide NAF zone in the Marmara region accommodates 24 mm/year dextral motion, with 70%-80% of this displacement taking place along the northern branch of the NAF, the Main Marmara Fault in the Sea of Marmara.

Orijinal dil	İngilizce
Ana bilgisayar yayını başlığı	Transform Plate Boundaries and Fracture Zones
Yayınlayan	Elsevier
Sayfalar	397-416
Sayfa sayısı	20
ISBN (Elektronik)	9780128120644
ISBN (Basılı)	9780128122464
DOI'lar	https://doi.org/10.1016/B978-0-12-812064-4.00016-5
Yayın durumu	Yayınlandı - 1 Oca 2018

Bibliyografik not

Publisher Copyright:
© 2019 Elsevier Inc. All rights reserved.

Belgeye Erişim

10.1016/B978-0-12-812064-4.00016-5

Diğer Dosyalar ve Linkler

Link to publication in Scopus

Alıntı Yap

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title = "Morphotectonics of the sea of marmara: Basins and highs on the north anatolian continental transform plate boundary",

abstract = "The Sea of Marmara is located in the North Anatolian Fault (NAF), a major continental transform plate boundary between the Eurasian and Anatolian-Aegean plates. The area is also under the influence of the N-S extensional Aegean regime. The 100 km-wide NAF zone in the Marmara region accommodates 24 mm/year dextral motion, with 70\%-80\% of this displacement taking place along the northern branch of the NAF, the Main Marmara Fault in the Sea of Marmara.",

keywords = "Aegean extension, Continental transform boundary, Morphotectonics, North anatolian fault, Sea of marmara, Transtensional basin evolution",

author = "\{Namık {\c C}ağatay\}, M. and G{\"u}lsen U{\c c}arku{\c s}",

year = "2018",

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doi = "10.1016/B978-0-12-812064-4.00016-5",

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TY - CHAP

T1 - Morphotectonics of the sea of marmara

T2 - Basins and highs on the north anatolian continental transform plate boundary

AU - Namık Çağatay, M.

AU - Uçarkuş, Gülsen

PY - 2018/1/1

Y1 - 2018/1/1

N2 - The Sea of Marmara is located in the North Anatolian Fault (NAF), a major continental transform plate boundary between the Eurasian and Anatolian-Aegean plates. The area is also under the influence of the N-S extensional Aegean regime. The 100 km-wide NAF zone in the Marmara region accommodates 24 mm/year dextral motion, with 70%-80% of this displacement taking place along the northern branch of the NAF, the Main Marmara Fault in the Sea of Marmara.

AB - The Sea of Marmara is located in the North Anatolian Fault (NAF), a major continental transform plate boundary between the Eurasian and Anatolian-Aegean plates. The area is also under the influence of the N-S extensional Aegean regime. The 100 km-wide NAF zone in the Marmara region accommodates 24 mm/year dextral motion, with 70%-80% of this displacement taking place along the northern branch of the NAF, the Main Marmara Fault in the Sea of Marmara.

KW - Aegean extension

KW - Continental transform boundary

KW - Morphotectonics

KW - North anatolian fault

KW - Sea of marmara

KW - Transtensional basin evolution

UR - https://www.scopus.com/pages/publications/85064229934

U2 - 10.1016/B978-0-12-812064-4.00016-5

DO - 10.1016/B978-0-12-812064-4.00016-5

M3 - Chapter

AN - SCOPUS:85064229934

SN - 9780128122464

SP - 397

EP - 416

BT - Transform Plate Boundaries and Fracture Zones

PB - Elsevier

ER -

Morphotectonics of the sea of marmara: Basins and highs on the north anatolian continental transform plate boundary

Özet

Bibliyografik not

Belgeye Erişim

Diğer Dosyalar ve Linkler

Parmak izi

Alıntı Yap