![]() The algorithms presented enable the automation of a spatial evaluation of b-value. ![]() ![]() The methods applied to evaluate the spatial variation of b-value and the algorithm for obtaining the magnitude of completeness and b-value for subsets of data are presented with some verification analyses. The interpretation of b-value as a parameter of rock mass response is discussed in this paper. The estimation of the spatial variation of the b-value of the Gutenberg-Richter relationship is important for both the general interpretation of the mechanism of rock mass response and seismic hazard assessment. 6TH SOUTHERN AFRICAN ROCK ENGINEERING SYMPOSIUMĮvaluation of the spatial variation of b-valueĪustralian Centrefor Geomechanics, The University of Western Australia, Australia
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