The July 20, 2017 M6. 6 Kos earthquake: seismic and geodetic evidence for an active north-dipping normal fault at the western end of the Gulf of Gökova (SE Aegean …

A Ganas, P Elias, V Kapetanidis, S Valkaniotis… - Pure and Applied …, 2019 - Springer
Abstract On July 20, 2017 22: 31 UTC, a strong M w= 6.6 earthquake occurred at shallow
depth between Kos Island (Greece) and Bodrum (Turkey). We derive a co-seismic fault …

[HTML][HTML] Marine Geotechnical Research in Greece: A Review of the Current Knowledge, Challenges and Prospects

NK Chtouris, T Hasiotis - Journal of Marine Science and Engineering, 2024 - mdpi.com
Greece is expanding its energy grid system with submarine power and fiber optic cables
between the mainland and the Aegean Sea islands. Additionally, pipelines have been …

The 20th July 2017 Bodrum–Kos Tsunami Field Survey

GG Dogan, A Annunziato, GA Papadopoulos… - Pure and Applied …, 2019 - Springer
Abstract The July 20, 2017 Bodrum–Kos Earthquake caused tsunami wave motions and
damage in the south of Bodrum Peninsula, Turkey, and on Kos Island, Greece. Immediately …

Slip distribution of the 2017 Mw6.6 Bodrum–Kos earthquake: resolving the ambiguity of fault geometry

AO Konca, SE Guvercin, S Ozarpaci… - Geophysical Journal …, 2019 - academic.oup.com
SUMMARY The 2017 July 20, M w6. 6 Bodrum–Kos earthquake occurred in the Gulf of
Gökova in the SE Aegean, a region characterized by N–S extension in the backarc of the …

Earthquake history of the Gökova fault zone by paleoseismologic trenching, SW Turkey

A Dikbaş, HS Akyüz, M Basmenji, E Kırkan - Natural Hazards, 2022 - Springer
The Gulf of Gökova is a half-graben that is located on the southernmost part of the Aegean
Extensional Region. The gulf is bounded on its north by the Gökova Fault Zone, which is an …

Impact on built and natural environment of the strong earthquakes of April 23, 1933, and July 20, 2017, in the southeast Aegean Sea, eastern Mediterranean

I Triantafyllou, GA Papadopoulos, E Lekkas - Natural Hazards, 2020 - Springer
Abstract The southeastern Aegean Sea is one of the most active areas in eastern
Mediterranean. On July 20, 2017, the area was inflicted by a strong earthquake (M w 6.6) …

The volcanic relief within the Kos-Nisyros-Tilos Tectonic Graben at the eastern edge of the Aegean volcanic arc, Greece and geohazard implications

P Nomikou, P Krassakis, S Kazana, D Papanikolaou… - Geosciences, 2021 - mdpi.com
The active Kos-Nisyros-Tilos volcanic field is located in the eastern sector of the Aegean
Volcanic Arc resulting from the subduction of the African plate beneath the Aegean plate …

Fault modelling, seismic sequence evolution and stress transfer scenarios for the July 20, 2017 (MW 6.6) Kos–Gökova Gulf earthquake, SE Aegean

S Sboras, I Lazos, E Mouzakiotis, V Karastathis… - Acta Geophysica, 2020 - Springer
Abstract The July 20, 2017, MW 6.6 Kos–Gökova Gulf earthquake occurred offshore, near
Bodrum of Turkey and Kos of Greece. It was one of the strongest in the broader area during …

Fault models for the Bodrum–Kos tsunamigenic earthquake (Mw6. 6) of 20 July 2017 in the east Aegean Sea

G Papadopoulos, A Agalos, M Charalampakis… - Journal of …, 2019 - Elsevier
We investigate a fault model for the shallow, strong (M w 6.6) tsunamigenic earthquake of 20
July 2017 with source area in the east Aegean Sea between Bodrum peninsula (Turkey) …

Simulation of the strong ground motion for the 20 July 2017 (Mw. 6.6) Bodrum–Kos earthquake

G Tanırcan, S Yelkenci-Necmioğlu - Bulletin of Earthquake Engineering, 2020 - Springer
A strong earthquake with Mw 6.6 occurred on 20 July, 2017 in Gökova Bay at the southwest
part of the Turkey, accompanied by a local tsunami which impacted Bodrum (Turkey) and …