Hagos, L.; Arvidsson, R.; Roberts, R. - In: Natural Hazards 39 (2006) 3, pp. 395-418
The region of interest is characterized by incomplete data sets and little information about the tectonic features. Therefore, two methodologies for estimating seismic hazard were used in order to elucidate the robustness of the results: the method of spatially smoothed seismicity introduced by...