Using the INGV (National Institute of Geophysics and Volcanology) seismic catalogue, nonextensive analysis of the instrumental seismicity of Italy was performed. The time span of the analyzed catalogue is from April 16, 2005 to March 31, 2009, and only events with magnitude M-L >= 1.9 were considered. The analysis of the spatial variation of the nonextensive parameters q and a was performed by means of scanning the Italian territory by a 1 degrees x 1 degrees spatial window, with a shift of 0.2 degrees in longitude and latitude. The nonextensive parameters were estimated by means of the Levenberg-Marquadt nonlinear least square fitting method, and the obtained results were checked for stability with the variation of a(0) and q(0), the initial values of the parameters in the fitting procedure. It was found that the q value is relatively low in areas, in which the strongest events (M-w>5.5 during the last 40 years) occurred. This finding could suggest that different earthquake triggering mechanisms govern the Italian seismicity, stick-slip-like where g is relatively low and fragment-asperity interaction-type where q is relatively high. Of course new analyses from different areas are needed in order to test such findings.
Analysis of Italian seismicity by using a nonextensive approach
Telesca L
2010
Abstract
Using the INGV (National Institute of Geophysics and Volcanology) seismic catalogue, nonextensive analysis of the instrumental seismicity of Italy was performed. The time span of the analyzed catalogue is from April 16, 2005 to March 31, 2009, and only events with magnitude M-L >= 1.9 were considered. The analysis of the spatial variation of the nonextensive parameters q and a was performed by means of scanning the Italian territory by a 1 degrees x 1 degrees spatial window, with a shift of 0.2 degrees in longitude and latitude. The nonextensive parameters were estimated by means of the Levenberg-Marquadt nonlinear least square fitting method, and the obtained results were checked for stability with the variation of a(0) and q(0), the initial values of the parameters in the fitting procedure. It was found that the q value is relatively low in areas, in which the strongest events (M-w>5.5 during the last 40 years) occurred. This finding could suggest that different earthquake triggering mechanisms govern the Italian seismicity, stick-slip-like where g is relatively low and fragment-asperity interaction-type where q is relatively high. Of course new analyses from different areas are needed in order to test such findings.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
