Comprehensive assessment of induced seismicity and its implications for the Atatürk dam: Insights from trenching, seismic investigations, and paleo-stress analysis along the Bozova fault in the East Anatolian tectonic regime, Southeast Türkiye

dc.contributor.authorKocbulut, Fikret
dc.contributor.authorSofta, Mustafa
dc.contributor.authorAkgun, Elif
dc.contributor.authorKosaroglu, Sinan
dc.contributor.authorEfe, Ahmet
dc.date.accessioned2026-08-12T17:11:01Z
dc.date.issued2025
dc.departmentFırat Üniversitesi
dc.description.abstractEarthquakes are predominantly associated with tectonically active regions, yet the rising frequency of seismic events globally has raised concerns about the role of industrial activities, such as fluid injection, conventional oil-gas, mining, and reservoir impoundment, in triggering significant earthquakes. While natural processes like tectonic stress changes, fluid migration, and surface loading are critical in earthquake nucleation, human-induced seismicity is becoming increasingly recognized. The Atat & uuml;rk Dam, T & uuml;rkiye's largest clay-core rockfill dam, situated near the East Anatolian Fault System, Adiyaman Fault Zone, and Bozova Fault, offers a compelling case to explore the interplay between tectonic and anthropogenic seismicity. This study presents the first trenching studies along the Bozova Fault, revealing evidence of surface ruptures and localized seismicity linked to reservoir impoundment and conventional oil and gas. Temporal and spatial analyses suggest that reservoir-induced mechanisms, including pore pressure diffusion and stress redistribution, significantly influence seismicity, recurrence interval, alongside dominant tectonic forces. By integrating trenching investigations, seismic analyses, and stress inversion techniques, this research highlights the critical role of anthropogenic factors in modulating seismic hazards. The findings emphasize the importance of paleoseismological and geophysical studies for distinguishing induced seismicity from natural tectonic activity, thereby contributing to improved seismic hazard assessment and mitigation strategies in tectonically active, reservoir-influenced regions.
dc.identifier.doi10.1007/s11629-024-9460-8
dc.identifier.endpage1225
dc.identifier.issn1672-6316
dc.identifier.issn1993-0321
dc.identifier.issue4
dc.identifier.orcid0000-0001-5064-9260
dc.identifier.orcid0000-0002-5989-4753
dc.identifier.orcid0000-0002-6556-2413
dc.identifier.orcid0000-0003-0274-9317
dc.identifier.scopus2-s2.0-105003306785
dc.identifier.scopusqualityQ1
dc.identifier.startpage1205
dc.identifier.urihttps://doi.org/10.1007/s11629-024-9460-8
dc.identifier.urihttps://hdl.handle.net/11508/50984
dc.identifier.volume22
dc.identifier.wosWOS:001473904400017
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherScience Press
dc.relation.ispartofJournal of Mountain Science
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20260511
dc.subjectInduced seismicity
dc.subjectBozova fault
dc.subjectAtat & uuml;rk dam
dc.subjectEarthquake mitigation
dc.titleComprehensive assessment of induced seismicity and its implications for the Atatürk dam: Insights from trenching, seismic investigations, and paleo-stress analysis along the Bozova fault in the East Anatolian tectonic regime, Southeast Türkiye
dc.typeArticle

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