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DOI | 10.1016/j.tecto.2020.228612 |
Modelling tectonic deformation along the North-Anatolian Fault in the Sea of Marmara | |
Bulkan S.; Vannucchi P.; Gasperini L.; Polonia A.; Cavozzi C. | |
发表日期 | 2020 |
ISSN | 00401951 |
卷号 | 794 |
英文摘要 | Using analogue techniques, we attempted to model the complex tectonic deformation pattern observed along the North-Anatolian Fault in the Sea of Marmara from morpho-bathymetry and seismic reflection images. In particular this paper focuses on the so-called Cinarcik segment of the fault connecting the eastern Izmit segment, which entirely ruptured during the Mw 7.4, 1999 earthquake, to the western segment of the Central High. The Çınarcık segment, potentially loaded after the Izmit earthquake, is expected to rupture during an earthquake occurring in the near future, possibly the next decades, with a high potential to affect the Istanbul metropolitan area. Our analysis suggests that the development of the observed structures accommodating strike-slip, transtensional and transpressional deformations, could be explained by changes in the geometry of fault segments within a right-lateral strike-slip tectonic regime. Tectonic deformations were reproduced in the analogue model by imposing a small (about 10°) and sharp difference in the relative orientations of the strike-slip segments at the edges of a major releasing bend. In the model slower strain accumulation occurs along the analogue of the Çınarcık segment than along the analogue of the Izmit segment of the fault. This would predict a delay for earthquakes triggered by stress transfer between the Izmit and Çınarcık segments. The model further predicts that most of the deformation in the Çınarcık basin is controlled by the sharp changes in the geometry of the fault itself. © 2020 Elsevier B.V. |
关键词 | Analogue modellingCinarcik basinFault orientationPull-apart basinsSea of MarmaraStress transfer |
英文关键词 | Deformation; Earthquakes; Analogue modeling; Izmit earthquakes; North Anatolian Fault; Relative orientation; Seismic reflections; Strain accumulations; Tectonic deformations; Transpressional deformation; Strike-slip faults; analog model; deformation; fault zone; pull apart basin; seismic reflection; stress analysis; strike-slip fault; tectonic evolution; tectonic setting; Cinarcik Basin; Sea of Marmara; Sea of Marmara; Turkey |
语种 | 英语 |
来源期刊 | Tectonophysics
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/207723 |
作者单位 | Earth Sciences Department, Royal Holloway, University of London, Egham, United Kingdom; Dipartimento di Scienze della Terra, Università degli Studi di Firenze, Via La Pira, 4, Firenze, Italy; Istituto di Scienze Marine-Consiglio Nazionale delle Ricerche (ISMAR), Bologna, IT-40129, Italy; NEXT – Natural and Experimental Tectonics research group, Department of Chemistry, Life Sciences and Environmental Sustainability, University of Parma, Italy |
推荐引用方式 GB/T 7714 | Bulkan S.,Vannucchi P.,Gasperini L.,et al. Modelling tectonic deformation along the North-Anatolian Fault in the Sea of Marmara[J],2020,794. |
APA | Bulkan S.,Vannucchi P.,Gasperini L.,Polonia A.,&Cavozzi C..(2020).Modelling tectonic deformation along the North-Anatolian Fault in the Sea of Marmara.Tectonophysics,794. |
MLA | Bulkan S.,et al."Modelling tectonic deformation along the North-Anatolian Fault in the Sea of Marmara".Tectonophysics 794(2020). |
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