Gelişmiş Arama

Basit öğe kaydını göster

dc.contributor.authorÖztürk, Serkan
dc.date.accessioned2019-12-10T11:51:05Z
dc.date.available2019-12-10T11:51:05Z
dc.date.issued2015
dc.identifier.issn2072-7151
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 Kutahya graben. In addition, the regions in which the lower b-values and the higher Z-values are estimated cover the Burdur fault zone, Aliaga-Dumlupinar faults and Bakircay grabens. Consequently, the relationships between seismic b-value, 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.en_US
dc.description.sponsorshipGumushane University Scientific Research Project (GUBAP, Turkey)Gumushane University [13.F5117.02.1]en_US
dc.description.sponsorshipThe author would like to thank to Prof. Dr. Stefan Weimer for providing ZMAP software and the reviewers, especially Ewald Bruckl, for their useful and constructive suggestions in improving this paper. I am grateful to Dr. Dogan Kalafat (KOERI) for providing us the earthquake catalogue. I also thank to KOERI for providing earthquake database via internet. This study is supported by Gumushane University Scientific Research Project (GUBAP, Turkey) with project no 13.F5117.02.1.en_US
dc.language.isoengen_US
dc.publisherOesterreichische Geologische Gesellschaften_US
dc.relation.ispartofAustrian Journal of Earth Sciencesen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subject[No Keywords]en_US
dc.titleA study on the correlations between seismotectonic b-value and Dc-value, and seismic quiescence Z-value in the Western Anatolian region of Turkeyen_US
dc.typearticleen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.description.wospublicationidWOS:000373403000008en_US
dc.description.scopuspublicationid2-s2.0-84981185505en_US
dc.departmentFakülteler, Mühendislik ve Doğa Bilimleri Fakültesi, Jeofizik Mühendisliği Bölümüen_US
dc.authoridÖztürk, Serkan / 0000-0003-1322-5164
dc.identifier.volume108en_US
dc.identifier.issue2en_US
dc.identifier.startpage172en_US
dc.identifier.endpage184en_US
dc.authorwosidÖztürk, Serkan / ABI-5194-2020
dc.authorscopusid57188980040


Bu öğenin dosyaları:

Thumbnail

Bu öğe aşağıdaki koleksiyon(lar)da görünmektedir.

Basit öğe kaydını göster