Show/Hide Menu
Hide/Show Apps
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Open Access Guideline
Open Access Guideline
Postgraduate Thesis Guideline
Postgraduate Thesis Guideline
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Guides
Guides
Thesis submission
Thesis submission
MS without thesis term project submission
MS without thesis term project submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Supporting Information
Supporting Information
General Information
General Information
Copyright, Embargo and License
Copyright, Embargo and License
Contact us
Contact us
The Samos Island (Aegean Sea) M7.0 earthquake: analysis and engineering implications of strong motion data
Date
2021-01-01
Author
Roumelioti, Zafeiria
Askan Gündoğan, Ayşegül
Sotiriadis, Dimitris
Gülerce, Zeynep
Melis, Nikolaos S.
Altindal, Abdullah
Akbaş, Burak
Sopaci, Eyüp
Karimzadeh, Shaghayegh
Kalogeras, Ioannis
Theodoulidis, Nikolaos
Konstantinidou, Kiriaki
Kale, Özkan
Margaris, Basil
Özacar, Atilla Arda
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
240
views
0
downloads
Cite This
We present a dataset of 77 strong ground motion records within 200 km epicentral distance from the 30 October 2020, M7.0 Samos Island (Aegean Sea) earthquake, which affected Greece and Turkey. Accelerograms from National Networks of both countries have been merged into a single dataset, including metadata that have been uniformly derived using a common preliminary source model. Initial findings from the analysis and comparative examination of acceleration time histories, Fourier amplitude spectra and 5%-damped response spectra are discussed along with significant source, propagation path and site effects. The long-period amplifications observed in most records in Izmir bay triggered failures and severe damages in weak structures. Yet, the spectral accelerations are observed to lie below the current and previous design spectra corresponding to the damaged regions. Peak ground motions are used to construct a purely instrumental-based macroseismic intensity map, which is capable of reflecting the actual earthquake damage caused by this considerably large event. Finally, peak ground motions are compared to various ground motion models (GMMs) and deviations are highlighted. Our overall preliminary analysis reveals a strong energy signature of the Samos earthquake in the period range 0.5–1.5 s at many sites, both on rock and soil, whereas records in the heavily hit Izmir city, at an epicentral distance circa 70 km, provide strong indication for additional amplification due to basin effects. At relatively large distance from the earthquake source (> 120 km), several recorded amplitudes are significantly lower than those predicted by many GMMs, implying that further studies are necessary toward the improvement of regional attenuation models.
Subject Keywords
Ground motion models
,
Macroseismic intensity
,
Samos earthquake 2020
,
Strong motion
URI
https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85118212586&origin=inward
https://hdl.handle.net/11511/94680
Journal
Bulletin of Earthquake Engineering
DOI
https://doi.org/10.1007/s10518-021-01251-5
Collections
Department of Civil Engineering, Article
Suggestions
OpenMETU
Core
The Chios, Greece Earthquake of 23 July 1949: Seismological Reassessment and Tsunami Investigations
Melis, Nikolaos S.; Okal, Emile A.; Synolakis, Costas E.; Kalogeras, Ioannis S.; Kanoğlu, Utku (Springer Science and Business Media LLC, 2020-03-01)
We present a modern seismological reassessment of the Chios earthquake of 23 July 1949, one of the largest in the Central Aegean Sea. We relocate the event to the basin separating Chios and Lesvos, and confirm a normal faulting mechanism generally comparable to that of the recent Lesvos earthquake located at the Northern end of that basin. The seismic moment obtained from mantle surface waves, M-0=7x10(26) dyn cm, makes it second only to the 1956 Amorgos earthquake. We compile all available macroseismic dat...
Characteristics of the 2020 Samos earthquake (Aegean Sea) using seismic data
Kiratzi, Anastasia; Papazachos, Costas; Özacar, Atilla Arda; PINAR, ALİ; Kkallas, Charis; Sopaci, Eyup (2021-01-01)
The 30 October 2020 Samos earthquake (Mw 7.0) ruptured an east–west striking, north dipping normal fault located offshore the northern coast of Samos Island, previously inferred from the bathymetry and regional tectonics. This fault, reported in the fault-databases as the North Samos and/or Kaystrios Fault, ruptured with almost pure dip-slip motion, in a region where both active extension and strike-slip deformation coexist. Historical information for the area confirms that similar ~ Mw7 events had also occ...
The 2017 July 20 M-w 6.6 Bodrum-Kos earthquake illuminates active faulting in the Gulf of Gokova, SW Turkey
Karasozen, Ezgi; Nissen, Edwin; Buyukakpinar, Pinar; CAMBAZ, MUSAVVER DİDEM; Kahraman, Metin; Ertan, Esra Kalkan; Abgarmi, Bizhan; Bergman, Eric; Ghods, Abdolreza; Özacar, Atilla Arda (2018-07-01)
The 2017 July 20 Bodrum-Kos earthquake (Mw 6.6) is the largest instrumentally recorded earthquake in the Gokova graben, one of the primary physiographic features of SW Turkey. Using seismology and satellite geodesy, we investigate its source characteristics, aftershock distribution, relationship with earlier instrumental seismicity, and association with known surface faulting. We show that the earthquake ruptured a planar (non-listric) normal fault that dips gently (similar to 37.) northwards beneath the no...
The role of site effects on elevated seismic demands and corollary structural damage during the October 30, 2020, M7.0 Samos Island (Aegean Sea) Earthquake
Altun, Selim; et. al. (2021-11-01)
On October 30, 2020 14:51 (UTC), a moment magnitude (M) 7.0 (USGS, EMSC) earthquake occurred in the Aegean Sea. This paper presents the reconnaissance findings regarding the site effects on recorded strong ground motion intensities and duration, along with the resulting induced-structural damage in Izmir Bay and Samos Island, respectively. In all rock records, relatively high intensity long period rock spectral accelerations were observed in the mid to long period range of 0.5-1.5 s, which are attributed to...
Reconnaissance of 2020 M 7.0 Samos Island (Aegean Sea) earthquake
Çetin, Kemal Önder; Sextos, Anastasios; Stewart, Jonathan P. (2021-08-01)
The Samos Island (Aegean Sea) Earthquake occurred on 30 October 2020. It produced a tsunami that impacted coastal communities, ground shaking that was locally amplified in some areas and that led to collapse of structures with 118 fatalities in both Greece and Turkey, and wide-ranging geotechnical effects including rockfalls, landsliding, and liquefaction. As a result of the global COVID-19 pandemic, the reconnaissance of this event did not involve the deployment of international teams, as would be typical ...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
Z. Roumelioti et al., “The Samos Island (Aegean Sea) M7.0 earthquake: analysis and engineering implications of strong motion data,”
Bulletin of Earthquake Engineering
, pp. 0–0, 2021, Accessed: 00, 2021. [Online]. Available: https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85118212586&origin=inward.