Complete data set of earthquakes in Turkey and the adjacent areas has been used in order to compute the x values in 24 seismic regions of Turkey. The parameter is obtained through Gumbel’s third asymptotic distribution of ...

In this study the properties of the aftershock sequences in the first five months after the 17 August 1999 'Izmit and 12 November 1999 D¨uzce earthquakes are investigated. For this purpose, the b-value of frequency-magnitude ...

This study was aimed at analysing the relationship between seismic b-value and fractal dimension Dc-value for Turkish epicentres. The earthquake catalogue consisting of 99,737 instrumentally-registered Turkish events was ...

In this study, we made an assessment of earthquake hazard parameters for different 24 source regions in and around Turkey. We used the seismic source zones and the database defined by Bayrak et al. [12] and Bayrak et al. ...

Characteristics of seismic activity from 1970 to 2010 along the North Anatolian Fault Zone (NAFZ) are analyzed to make a statistical assessment by using the Gutenberg-Richter b-value, seismic quiescence Z-value, fractal ...

Characteristics of seismic activity along the North Anatolian Fault Zone are analyzed between 1970 and 2010. Magnitude completeness changes between 2.7 and 2.9 in the North Anatolian Fault Zone. The frequency-magnitude ...

Aftershock sequences of the magnitude MW ¼6.4 Bingo¨l earthquake of 1 May, 2003 (Turkey) are studied to analyze the spatial and temporal variability of seismicity parameters of the b value of the frequencymagnitude ...

Several catalogues of global earthquakes reported for the time period from 1900 to 2000 have been compiled to examine lateral variations of the modal (a/b) values as derived from the Gutenberg–Richter empirical law. For ...

The variations of seismicity rate changes prior to the occurrence of 1 May 2003 Bingöl earthquake has been analyzed by statistical method, with the observation of pointing up precursory seismic sequence. We investigated ...

Statistical properties of the aftershock sequence of July 4, 2018 earthquake, ML=5.1, near Durrës, Albania are here described in time, space and magnitude by means of pvalue, Dc-value and b-value, respectively. We used ...