TY - JOUR T1 - Orta Anadolu Bölgesi ve Civarındaki Depremselliğin Bölge-Zaman-Magnitüd Analizleri ve Güncel Deprem Potansiyeli TT - Region-Time-Magnitude Analyses of the Seismicity in and around the Central Anatolian Region and Current Earthquake Potential AU - Öztürk, Serkan PY - 2019 DA - December DO - 10.46464/tdad.644126 JF - Türk Deprem Araştırma Dergisi JO - TDAD PB - Afet ve Acil Durum Yönetimi Başkanlığı (AFAD) WT - DergiPark SN - 2687-301X SP - 148 EP - 166 VL - 1 IS - 2 LA - tr AB - Bu çalışmanın amacı, Türkiye’nin Orta Anadolu Bölgesi vecivarındaki deprem oluşumlarının detaylı istatistiksel analizlerini yapmak vegelecekteki olası deprem bölgelerini tahmin etmektir. Bu kapsamda, Mc-değeri,b-değeri, Dc-değeri, Z-değeri gibi sismotektonik değişkenlerinbölge-zaman-magnitüd analizleri yapılarak, güncel/gelecek deprem potansiyeliortaya konulmuştur. Mc=2.6 alınarak b=1.26±0.07 olarak hesaplanmıştır. Bu büyükdeğer küçük magnitüdlü depremlerin baskın olduğuna işaret etmektedir. Dc-değeri1.31±0.03 olarak hesaplanmıştır ve bu nispeten küçük değer, episantrlararasındaki uzaklığın kümelenme çapına yaklaştığını ve deprem aktivitesinin dahaküçük ölçeklerde veya daha büyük alanlarda kümelendiğini göstermektedir. 2019yılı başında düşük b-değerli ve yüksek Z-değerli anomali bölgeleri, Tuz Gölü FayZonu ve civarında, Orta Anadolu Fay Zonunda, Salanda ve Niğde faylarındagözlenmiştir. Önemli bir sonuç olarak, bu bölgeler gelecekteki büyük/güçlüdepremler için en olası bölgeler olarak düşünülebilir. KW - Orta Anadolu KW - b-değeri KW - Dc-değeri KW - Z-değeri KW - Deprem potansiyeli N2 - The purpose of this study is to make detailedstatistical analyses of earthquake occurrences in and around the CentralAnatolian Region of Turkey and to forecast the possible earthquake regions inthe future. In this scope, by performing the region-time-magnitude analyses ofseismotectonic variables such as Mc-value, b-value, Dc-value, Z-value, thecurrent/future earthquake potential was defined. b-value was computed as 1.26±0.07by taking Mc=2.6 and this large value indicates that the earthquakes with smallmagnitude are dominant. Dc-value was calculated as 1.31±0.03 and thisrelatively small value shows that distance between the epicenters approachesthe diameter of cluster, and earthquake activity is more clustered in largerregions/at smaller scales. Anomaly regions with low b-value and large Z-valueat the beginning of 2019 were found in and around Tuz Gölü Fault Zone, CentralAnatolian Fault Zone, Salanda and Niğde faults. As an important result, theseregions may be considered as the most likely regions for strong/largeearthquakes in the future. CR - Ali S.M., 2016. Statistical analysis of seismicity in Egypt and its surroundings, Arab. J. Geosci. 9, 52, doi.org/10.1007/s12517-015-2079-x. 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Seismic quiescence before the M7, 1988, Spitak earthquake, Armenia, Geophys. J. Int. 134, 329-340. UR - https://doi.org/10.46464/tdad.644126 L1 - https://dergipark.org.tr/tr/download/article-file/888050 ER -