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Full-Text Articles in Tectonics and Structure
The Relation Of Seismic Velocity And Attenuation Pattern In The East Anatolian Fault Zone With Earthquake Occurrence: Example Of January 24, 2020 Sivrice Earthquake, Şakir Şahi̇n, Erdinç Öksüm
The Relation Of Seismic Velocity And Attenuation Pattern In The East Anatolian Fault Zone With Earthquake Occurrence: Example Of January 24, 2020 Sivrice Earthquake, Şakir Şahi̇n, Erdinç Öksüm
Bulletin of the Mineral Research and Exploration
The East Anatolian Fault Zone (EAFZ) is one the main tectonic elements of Turkey, which borders the Anatolian plate from the east. EAFZ, which is NE - SW direction, consists of many fault segments. In the historical and instrumental period, many damaging earthquakes occurred, the largest being 6.8 (Ms) as the 1971 Bingöl earthquake. The last magnitude 6.6 (Ml) (Mw=6.8) earthquake occurred on January 24, 2020 in Elazığ-Sivrice Hazar-Sincik segment of EAFZ. However, considering the historical and instrumental activity, it is seen that many fault segments are silent. In this study, the silent and active segments, and their seismic velocity …