Araştırma Makalesi
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Yıl 2021, Cilt: 166 Sayı: 166, 85 - 112, 15.12.2021
https://doi.org/10.19111/bulletinofmre.984922

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Kaynakça

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Active tectonics of Gülpınar-Tuzla area (Biga Peninsula, NW Turkey): the source of 6 February-24 March 2017 earthquake cluster

Yıl 2021, Cilt: 166 Sayı: 166, 85 - 112, 15.12.2021
https://doi.org/10.19111/bulletinofmre.984922

Öz

The variation in the motion sense of Anatolian platelet in Aegean Sea resulted in a strike-slip tectonic regime and related neotectonic domain, the central to northern Aegean neotectonic province, which also includes both western Marmara Sea and Biga Peninsula. Our study focuses mostly on the Gülpınar-Tuzla earthquake area located at the southwestern tip of Biga Peninsula, which is controlled by the southern major strand of the North Anatolian Fault System (NAFS). The strand consists of two sections, the onshore Biga and offshore Babakale-Skyros sections. Both sections are seismically very active. The Gülpınar-Tuzla earthquake area is composed of the Paleozoic metamorphic rocks, the Oligo-Miocene granitoid pluton, Lower-Middle Miocene calc-alkalic volcanic rocks and the Upper Miocene-Pliocene sedimentary sequence. All of these rocks, which formed and deformed (folded to tilted) in palaeotectonic period, are overlain with an angular unconformity by the Quaternary neotectonic basin fill, that is nearly flat-lying except for the faulted basin margins. Both the onshore and offshore sections of the southern strand are linked to each other in terms of the structures characterizing the Babakale pull-apart basin and the Gülpınar-Tuzla earthquake area. The latter is shaped by the NE-trending Gülpınar (GFZ) and Yenice-Gönen Fault Zone (YGFZ), the ENE-trending Edremit fault zone (EFZ), the WNW-trending Tuzla Fault Zone (TFZ) and three strike-slip basins (Ayvacık, Behramkale and Tuzla basins) developed along them. Some segments of both the TFZ and GFZ were reactivated by the occurrences of seven moderate-to small-sized independent earthquakes and related aftershocks over 2760. Five of the independent earthquakes have an origin of oblique-slip normal faulting, while the rest two seismic events are strike-slip faulting in origin. Focal mechanism solution diagrams of these two groups of earthquakes reveal that the Gülpınar-Tuzla area is under the control of a strike-slip neotectonic regime, which commenced in Early Quaternary time owing to the major inversion in extensional palaeotectonic regime. This is also supported by the palaeostress analysis of slip-plane data measured on fault slickensides. The uniform slip rates on both the YGFZ and EFZ are 10.8 mm/yr and 7.3 mm/yr, respectively.

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  • Yılmaz, Y., Genç, S.C., Gürer, F., Bozcu, M., Yılmaz, K., Karacık, Z., Altunkaynak, S., Elmas, A. 2000. When did the Western Anatolian grabens begin to develop? Geological Society of London, Special Publications 173, 353-384.
Toplam 111 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

Ali Koçyiğit Bu kişi benim 0000-0002-0026-2831

Şule Gürboğa Bu kişi benim 0000-0002-5225-5895

Yayımlanma Tarihi 15 Aralık 2021
Yayımlandığı Sayı Yıl 2021 Cilt: 166 Sayı: 166

Kaynak Göster

APA Koçyiğit, A., & Gürboğa, Ş. (2021). Active tectonics of Gülpınar-Tuzla area (Biga Peninsula, NW Turkey): the source of 6 February-24 March 2017 earthquake cluster. Bulletin of the Mineral Research and Exploration, 166(166), 85-112. https://doi.org/10.19111/bulletinofmre.984922
AMA Koçyiğit A, Gürboğa Ş. Active tectonics of Gülpınar-Tuzla area (Biga Peninsula, NW Turkey): the source of 6 February-24 March 2017 earthquake cluster. Bull.Min.Res.Exp. Aralık 2021;166(166):85-112. doi:10.19111/bulletinofmre.984922
Chicago Koçyiğit, Ali, ve Şule Gürboğa. “Active Tectonics of Gülpınar-Tuzla Area (Biga Peninsula, NW Turkey): The Source of 6 February-24 March 2017 Earthquake Cluster”. Bulletin of the Mineral Research and Exploration 166, sy. 166 (Aralık 2021): 85-112. https://doi.org/10.19111/bulletinofmre.984922.
EndNote Koçyiğit A, Gürboğa Ş (01 Aralık 2021) Active tectonics of Gülpınar-Tuzla area (Biga Peninsula, NW Turkey): the source of 6 February-24 March 2017 earthquake cluster. Bulletin of the Mineral Research and Exploration 166 166 85–112.
IEEE A. Koçyiğit ve Ş. Gürboğa, “Active tectonics of Gülpınar-Tuzla area (Biga Peninsula, NW Turkey): the source of 6 February-24 March 2017 earthquake cluster”, Bull.Min.Res.Exp., c. 166, sy. 166, ss. 85–112, 2021, doi: 10.19111/bulletinofmre.984922.
ISNAD Koçyiğit, Ali - Gürboğa, Şule. “Active Tectonics of Gülpınar-Tuzla Area (Biga Peninsula, NW Turkey): The Source of 6 February-24 March 2017 Earthquake Cluster”. Bulletin of the Mineral Research and Exploration 166/166 (Aralık 2021), 85-112. https://doi.org/10.19111/bulletinofmre.984922.
JAMA Koçyiğit A, Gürboğa Ş. Active tectonics of Gülpınar-Tuzla area (Biga Peninsula, NW Turkey): the source of 6 February-24 March 2017 earthquake cluster. Bull.Min.Res.Exp. 2021;166:85–112.
MLA Koçyiğit, Ali ve Şule Gürboğa. “Active Tectonics of Gülpınar-Tuzla Area (Biga Peninsula, NW Turkey): The Source of 6 February-24 March 2017 Earthquake Cluster”. Bulletin of the Mineral Research and Exploration, c. 166, sy. 166, 2021, ss. 85-112, doi:10.19111/bulletinofmre.984922.
Vancouver Koçyiğit A, Gürboğa Ş. Active tectonics of Gülpınar-Tuzla area (Biga Peninsula, NW Turkey): the source of 6 February-24 March 2017 earthquake cluster. Bull.Min.Res.Exp. 2021;166(166):85-112.

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