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- W4322006786 abstract "The island of Crete is located in the Southern Aegean Sea, at the central part of the Hellenic Trench. The increased seismic activity in the region as a result of the convergence of the Eurasian and African tectonic plates highlights the importance of improving our knowledge on local seismotectonic features that play a key role in the seismic hazard. In this work, we used over than 1400 manually revised events from 2018 to 2022 in order to obtain both local and regional 1-D velocity models. The final output was put into the Seismic Inversion procedure, using body-wave (P, S) travel-time data in order to perform a detailed analysis and correlation of medium to large-scale (in km) anomalies with the activation of local and regional faults. Crete's central region exhibited complex shallow structures, whereas in deeper tomographic slices (> 40 km depth) a smoother, more continuous image, was revealed. This result may have been caused by the upward migration of fluids due to the subduction of Tethys oceanic lithosphere. As a result of the final dataset analysis, and exploring the most recent aftershock sequences (e.g. 2021-2022 Arkalochorion earthquakes) the research area's prevailing seismotectonic processes were investigated in more detail, clarifying the relationship between shallow and intermediate-depth earthquake activity. Acknowledgements: This work was supported by the Hellenic Mediterranean University, contract 104/18-10-2022, in the frames of the «Study of GEophysicalsystems and their laboratory equivalents towards the understanding Of Earthquake Early Warning Systems (GEOWS)». " @default.
- W4322006786 created "2023-02-26" @default.
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- W4322006786 date "2023-05-15" @default.
- W4322006786 modified "2023-09-30" @default.
- W4322006786 title "Investigation of 1-D and 3-D Crustal seismic velocity structure in the broader area of Crete (Greece)" @default.
- W4322006786 doi "https://doi.org/10.5194/egusphere-egu23-6588" @default.
- W4322006786 hasPublicationYear "2023" @default.
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