A study on the correlations between seismotectonic b-value and Dc-value, and seismic quiescence Z-value in the western anatolian region of Turkey

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Özet

The Western Anatolian region is one of the most seismically active sectors of Turkey where small-magnitude events with considerable clustering occur frequently. The spatial and temporal behaviors of seismic activity as quantified by the fractal dimension Dc-value, seismotectonic b-value and seismic quiescence Z-value are investigated for the Western Anatolian region. For this purpose, a statistical relationship is developed between b and Dc-values, and regional and temporal changes of these parameters are analyzed in order to reveal the potential of future earthquakes in the study region. By using standard deviate Z-value, current seismicity rate changes are estimated in the beginning of 2014. The Western Anatolian region is divided into 18 different seismogenic subregions. Orthogonal regression fit is preferred in order to estimate more up-to-date and reliable statistical correlation between two seismotectonic parameters. The relationship of Dc=2.74-0.29*b is computed with a significant negative correlation (r = -0.73) between b and Dc-values for the Western Anatolian earthquake distributions. There are clear fluctuations in the temporal changes of these two parameters and the same results are relatively obtained in previous studies in literature. Lower b-values smaller than 1.0 and also higher Dc-value are observed in the Burdur fault zone and Kütahya graben. In addition, the regions in which the lower b-values and the higher Z-values are estimated cover the Burdur fault zone, Aliağa-Dumlupınar faults and Bakırçay grabens. Consequently, the relationships between seismic bvalue, fractal dimension Dc-value and seismic quiescence Z-value may provide important evidences to put forth the next earthquake potential in Western Anatolia. In addition, monitoring of microseismic activity and behaviors of some other geophysical parameters should be analyzed in space and time and evaluated carefully.

Anahtar Kelimeler

RDL Kalıcı Bağlantı (PID)
https://rdlopen.rawdatalibrary.net/r/gumushane/15742Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.17738/ajes.2015.0019Yayıncı resmi DOI adresi
Tam Kayıt
AlanDeğerDil
dc.contributor.authorÖztürk, Serkan
dc.date.accessioned2026-10-22T10:24:28.294088076Z
dc.date.available2026-10-22T10:24:28.294088076Z
dc.date.issued2015
dc.description.abstractThe Western Anatolian region is one of the most seismically active sectors of Turkey where small-magnitude events with considerable clustering occur frequently. The spatial and temporal behaviors of seismic activity as quantified by the fractal dimension Dc-value, seismotectonic b-value and seismic quiescence Z-value are investigated for the Western Anatolian region. For this purpose, a statistical relationship is developed between b and Dc-values, and regional and temporal changes of these parameters are analyzed in order to reveal the potential of future earthquakes in the study region. By using standard deviate Z-value, current seismicity rate changes are estimated in the beginning of 2014. The Western Anatolian region is divided into 18 different seismogenic subregions. Orthogonal regression fit is preferred in order to estimate more up-to-date and reliable statistical correlation between two seismotectonic parameters. The relationship of Dc=2.74-0.29*b is computed with a significant negative correlation (r = -0.73) between b and Dc-values for the Western Anatolian earthquake distributions. There are clear fluctuations in the temporal changes of these two parameters and the same results are relatively obtained in previous studies in literature. Lower b-values smaller than 1.0 and also higher Dc-value are observed in the Burdur fault zone and Kütahya graben. In addition, the regions in which the lower b-values and the higher Z-values are estimated cover the Burdur fault zone, Aliağa-Dumlupınar faults and Bakırçay grabens. Consequently, the relationships between seismic bvalue, fractal dimension Dc-value and seismic quiescence Z-value may provide important evidences to put forth the next earthquake potential in Western Anatolia. In addition, monitoring of microseismic activity and behaviors of some other geophysical parameters should be analyzed in space and time and evaluated carefully.
dc.description.sponsorshipGumushane University Scientific Research Project (GUBAP, Turkey) [13.F5117.02.1]
dc.identifier.doi10.17738/ajes.2015.0019
dc.identifier.endpage184
dc.identifier.issn0251-7493
dc.identifier.issue2
dc.identifier.scopus2-s2.0-84981185505
dc.identifier.startpage172
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/15742
dc.identifier.volume108
dc.identifier.wosWOS:000373403000008
dc.language.isoen
dc.publisherAustrian Geological Society
dc.relation.ispartofAustrian Journal of Earth Sciences
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectB-value
dc.subjectFractal dimension
dc.subjectSeismic quiescence
dc.subjectWestern Anatolian region
dc.subject.classificationGeosciences, Multidisciplinary
dc.subject.classificationGeology
dc.subject.otherAnatolia
dc.subject.otherTurkey
dc.subject.otheractive fault
dc.subject.othercorrelation
dc.subject.otherdisaster management
dc.subject.otherearthquake prediction
dc.subject.otherfault zone
dc.subject.otherfuture prospect
dc.subject.otherseismic quiescence
dc.subject.otherseismicity
dc.subject.otherseismotectonics
dc.subject.othertectonic setting
dc.titleA study on the correlations between seismotectonic b-value and Dc-value, and seismic quiescence Z-value in the western anatolian region of Turkey
dc.typeArticle
dspace.entity.typePublication
rdl.citation.openalex28
rdl.citation.scopus34
rdl.citation.wos22
rdl.oa.statusgold
rdl.oa.statusclosed
rdl.source.indexSCOPUS
rdl.source.indexWOS
rdl.wos.indexScience Citation Index Expanded (SCI-EXPANDED)