- Open Access
Spatial and temporal variations of the aftershock sequences of the 1999 İzmit and Düzce earthquakes
© The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2004
Received: 10 February 2003
Accepted: 27 September 2004
Published: 20 June 2014
In this study the properties of the aftershock sequences in the first five months after the 17 August 1999 İzmit and 12 November 1999 Düzce earthquakes are investigated. For this purpose, the b-value of frequency-magnitude distribution of earthquakes and temporal decay rate of aftershocks as described by the p-value in the modified Omori law are calculated. The data taken from the website of the KOERI consist of 1841 events for the İzmit and 913 events for the Düzce activity, respectively. The b-value for the İzmit sequence is found as 1.10±0.03 with Mc = 2.6 and b = 1.16 ± 0.05 for the Düzce sequence with Mc = 2.8. Both b-values are close to 1 and typical for aftershock sequences. The p-values are calculated as 0.86 ± 0.05 for the İzmit and p = 1.34 ± 0.09 for Düzce aftershocks, respectively. Small p-value found in İzmit sequence may be a result of the background seismicity of the aftershock region. Because of the lower p-value for the İzmit activity than that of the Düzce sequence, the aftershocks show a relatively slow decay rate in the İzmit earthquake. Considerable spatial variability is found, b-values ranging from 0.8 to 1.6, and p-values ranging from 0.4 to 1.4. The spatial variations of b and p-values of an aftershock sequence may associate with the rupture mechanism and geological structure of an earthquake area. A good agreement between the slip and b-value for the Düzce sequence are found whereas we could not observe a linear relation between these parameters for the İzmit sequence. After the İzmit earthquake, the larger b-values correlate with the regions where the lower stress changes occurred whereas the lower b-values are in the areas with the larger stress variations. Also, the lower and higher b-values are related to the higher and lower P-wave velocity in general. Regarding the geological aspect, the larger b and p-values for the two sequences are related to Holocene alluvium structures which have low velocity. On the other hand, after the both earthquakes, the larger p-values correlate well with the regions on which the maximum slip is located and the lower p-values are related to the lower slip regions. However, the material properties seem more effective than the stress changes and slip distributions in the b-value variations and the slip distribution is the most significant factor on p-values in the both sequences.