Geological evolution of the Gulf of Saros, NE Aegean Sea

M. N. Çaǧatay; N. Görür; B. Alpar; R. Saatçilar; R. Akkök; M. Sakinç; H. Yüce; C. Yaltirak; I. Kuşcu

doi:10.1007/s003670050045

Geological evolution of the Gulf of Saros, NE Aegean Sea

M. N. Çaǧatay^*
, N. Görür
, B. Alpar
, R. Saatçilar
, R. Akkök
, M. Sakinç
, H. Yüce
, C. Yaltirak
, I. Kuşcu

^*Bu çalışma için yazışmadan sorumlu yazar

Jeoloji Mühendisliği Bölümü

I.U. Müşküle Sokak
Istanbul Technical University
Scientific and Technological Research Council of Turkey
Hydrography Oceanogr.
Maden Tetkik ve Arama Genel Mudurlugu

Araştırma sonucu: Dergiye katkı › Makale › bilirkişi

54 Atıf (Scopus)

Özet

The Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic régime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.

Orijinal dil	İngilizce
Sayfa (başlangıç-bitiş)	1-9
Sayfa sayısı	9
Dergi	Geo-Marine Letters
Hacim	18
Basın numarası	1
DOI'lar	https://doi.org/10.1007/s003670050045
Yayın durumu	Yayınlandı - 1998

Belgeye Erişim

10.1007/s003670050045

Diğer Dosyalar ve Linkler

Link to publication in Scopus

Alıntı Yap

@article{571e94f0551a440f98e307967511db4f,

title = "Geological evolution of the Gulf of Saros, NE Aegean Sea",

abstract = "The Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic r{\'e}gime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.",

author = "{\c C}aǧatay, \{M. N.\} and N. G{\"o}r{\"u}r and B. Alpar and R. Saat{\c c}ilar and R. Akk{\"o}k and M. Sakin{\c c} and H. Y{\"u}ce and C. Yaltirak and I. Ku{\c s}cu",

year = "1998",

doi = "10.1007/s003670050045",

language = "English",

volume = "18",

pages = "1--9",

journal = "Geo-Marine Letters",

issn = "0276-0460",

publisher = "Springer Verlag",

number = "1",

}

TY - JOUR

T1 - Geological evolution of the Gulf of Saros, NE Aegean Sea

AU - Çaǧatay, M. N.

AU - Görür, N.

AU - Alpar, B.

AU - Saatçilar, R.

AU - Akkök, R.

AU - Sakinç, M.

AU - Yüce, H.

AU - Yaltirak, C.

AU - Kuşcu, I.

PY - 1998

Y1 - 1998

N2 - The Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic régime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.

AB - The Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic régime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.

UR - https://www.scopus.com/pages/publications/0031852249

U2 - 10.1007/s003670050045

DO - 10.1007/s003670050045

M3 - Article

AN - SCOPUS:0031852249

SN - 0276-0460

VL - 18

SP - 1

EP - 9

JO - Geo-Marine Letters

JF - Geo-Marine Letters

IS - 1

ER -

Geological evolution of the Gulf of Saros, NE Aegean Sea

Özet

Belgeye Erişim

Diğer Dosyalar ve Linkler

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