Newly discovered, the Kayapa-Yenis,ehir cross-basin fault: As revealed by geological and geophysical studies along the southern branch of the North Anatolian Fault Zone, a possible source of the destructive 1855 Bursa earthquakes

被引：1

作者：

Seyitoglu, Gurol ^{[1
]}

Esat, Korhan ^{[1
]}

Tun, Muammer ^{[2
]}

Oruc, Bulent ^{[3
]}

Peksen, Ertan ^{[3
]}

Aktug, Bahadir ^{[4
]}

Kaypak, Bulent ^{[2
]}

Koca, Begum ^{[2
,4
]}

Balkan, Emir ^{[2
]}

Mutlu, Sunay ^{[2
]}

Pekkan, Emrah ^{[2
]}

Cetinkaya, Delal ^{[1
]}

机构：

[1] Ankara Univ, Dept Geol Eng, Tecton Res Grp, Ankara, Turkiye

[2] Eskisehir Tech Univ, Inst Earth & Space Sci, Eskisehir, Turkiye

[3] Kocaeli Univ, Dept Geophys Eng, Kocaeli, Turkiye

[4] Ankara Univ, Dept Geophys Eng, Ankara, Turkiye

来源：

JOURNAL OF STRUCTURAL GEOLOGY | 2024年 / 179卷

关键词：

PULL-APART BASINS; WESTERN ANATOLIA; MARMARA; DEFORMATION; REGION; EXTINCTION; EVOLUTION; SEA; SEISMICITY; MODELS;

D O I：

10.1016/j.jsg.2023.105028

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

This study presents our geological and geophysical findings about a right-lateral cross-basin fault (Kayapa-Yenis,ehir Fault-KYF) formed in the composite Bursa-west, Bursa-east, and Yenis,ehir pull-apart basins on the southern branch of the North Anatolian Fault Zone around Bursa in southern Marmara. We examined the compatibility of our observations with various models proposed in the literature. The right-lateral KYF has slip rates of a maximum of 8.8 mm/year and a minimum of 3.0 mm/year, according to our GPS-based block modeling, and it seems to be related to the latest destructive 1850 and 1855 earthquakes around Bursa. The damage distribution of these earthquakes allows interpretation that only the western part of the KYF was ruptured. The slip rates obtained from the block modeling combined with 621 years since a 1400 CE earthquake suggest that 5.5 m of displacement has accumulated on the eastern 55 km of the KYF. These parameters suggest a magnitude 7.0 or greater earthquake is possible.

引用

页数：14