Spatial and temporal analysis of current seismic quiescence in the east anatolian fault zone, Eastern Part of Turkey

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In the scope of this study, an evaluation of recent seismic quiescence in the East Anatolian Fault Zone, eastern part of Turkey, is made by using the standard deviate Z-value. For this purpose, a statistical assessment of the spatial and temporal variations of the seismicity rate changes in the beginning of 2013is performed by using ZMAP software package. Results show that four areas with an apparently seismic quiescence may be important in the East Anatolian Fault Zone in the beginning of 2013. These anomalies are observed centered at 39.48°N-39.712°E (between Ovacik and Pülümür, Tunceli), the second one is found centered at 39.06°N-40.297°E (including Karakoçan, Sancak-Uzunpinar and Göynük fault zones), the third one is found centered at 38.55°N-38.763°E (between Malatya fault and EAFZ, north of Pötürge, Malatya) and the last one is found centered as 39.95°N-35.647°E (between Ceyhan-Yumurtalik-Karatas, Adana). The beginnings of these seismic quiescence anomalies are recently observed and nearly started in the beginning of 2007.For this reason, special attention should be given to these regions where the seismic quiescence is observed.

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https://rdlopen.rawdatalibrary.net/r/gumushane/15710Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.3997/2214-4609.20141967Yayıncı resmi DOI adresi
Tam Kayıt
AlanDeğerDil
dc.contributor.authorÖztürk, S.
dc.contributor.authorSariçiçek, I.
dc.date.accessioned2026-10-22T10:24:25.245926942Z
dc.date.available2026-10-22T10:24:25.245926942Z
dc.date.issued2014
dc.description.abstractIn the scope of this study, an evaluation of recent seismic quiescence in the East Anatolian Fault Zone, eastern part of Turkey, is made by using the standard deviate Z-value. For this purpose, a statistical assessment of the spatial and temporal variations of the seismicity rate changes in the beginning of 2013is performed by using ZMAP software package. Results show that four areas with an apparently seismic quiescence may be important in the East Anatolian Fault Zone in the beginning of 2013. These anomalies are observed centered at 39.48°N-39.712°E (between Ovacik and Pülümür, Tunceli), the second one is found centered at 39.06°N-40.297°E (including Karakoçan, Sancak-Uzunpinar and Göynük fault zones), the third one is found centered at 38.55°N-38.763°E (between Malatya fault and EAFZ, north of Pötürge, Malatya) and the last one is found centered as 39.95°N-35.647°E (between Ceyhan-Yumurtalik-Karatas, Adana). The beginnings of these seismic quiescence anomalies are recently observed and nearly started in the beginning of 2007.For this reason, special attention should be given to these regions where the seismic quiescence is observed.
dc.identifier.doi10.3997/2214-4609.20141967
dc.identifier.isbn978-946282027-2
dc.identifier.scopus2-s2.0-85087239889
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/15710
dc.language.isoen
dc.publisherEuropean Association of Geoscientists and Engineers, EAGE
dc.relation.conference20th European Meeting of Environmental and Engineering Geophysics of EAGE's Near Surface Geoscience Division
dc.relation.ispartofNear Surface Geoscience 2014 - 20th European Meeting of Environmental and Engineering Geophysics
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subject.otherEngineering
dc.subject.otherGeology
dc.subject.otherGeophysics
dc.subject.otherIndustrial engineering
dc.subject.otherFault zone
dc.subject.otherSpatial and temporal analysis
dc.subject.otherSpatial and temporal variation
dc.subject.otherStatistical assessment
dc.subject.otherZ value
dc.subject.otherSeismology
dc.titleSpatial and temporal analysis of current seismic quiescence in the east anatolian fault zone, Eastern Part of Turkey
dc.typeConference Object
dspace.entity.typePublication
rdl.citation.openalex0
rdl.citation.scopus0
rdl.conference.date14 September 2014 through 18 September 2014
rdl.conference.placeAthens
rdl.oa.statusclosed
rdl.source.indexSCOPUS