Time-series analysis of water and soil radon anomalies to identify micro-macro-earthquakes

dc.contributor.authorKulahci, Fatih
dc.contributor.authorCicek, Serif
dc.date.accessioned2026-08-12T16:40:18Z
dc.date.issued2015
dc.departmentFırat Üniversitesi
dc.description.abstractSoil and water Rn-222 gas concentrations were observed over 8 months on a branch of the East Anatolian Fault Zone (EAFZ), which is one of the world's most seismically active areas. During such observations, 110 micro-and macro-earthquakes were recorded. The largest earthquake was the ML 5.4 Icme earthquake that occurred on 23 June 2011. Twenty days before this earthquake, anomalous increases were recorded in soil and water Rn-222 gas as a time-series. The Rn-222 anomalies recorded in the research area were likely precursors to the Icme earthquake. A few days before the earthquake, the soil and water Rn-222 gas concentrations increased by approximately 70-99 %. Consequently, strong evidence suggests that the radon anomaly originated due to stress accumulation preceding the Icme earthquake.
dc.identifier.doi10.1007/s12517-014-1513-9
dc.identifier.endpage5246
dc.identifier.issn1866-7511
dc.identifier.issn1866-7538
dc.identifier.issue7
dc.identifier.orcid0000-0001-6566-4308
dc.identifier.scopus2-s2.0-84933677829
dc.identifier.scopusqualityN/A
dc.identifier.startpage5239
dc.identifier.urihttps://doi.org/10.1007/s12517-014-1513-9
dc.identifier.urihttps://hdl.handle.net/11508/45346
dc.identifier.volume8
dc.identifier.wosWOS:000357101200071
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherSpringer Heidelberg
dc.relation.ispartofArabian Journal of Geosciences
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20260511
dc.subjectRadon
dc.subjectPrecursor
dc.subjectMicro-earthquake
dc.subjectTrend analysis
dc.subjectTime-series
dc.subjectPrediction
dc.titleTime-series analysis of water and soil radon anomalies to identify micro-macro-earthquakes
dc.typeArticle

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