Figure 2From: Coseismic visibility of a small fragile patch involved in the rupture of a large patch - implications from fully dynamic rate-state earthquake sequence simulations producing variable manners of earthquake initiation Event statistics for different scale ratios. Statistics of types of earthquakes in simulations conducted by Noda et al. (2013a). (a) Types of L events. As the scale ratio α increases, less and less L events are generated by cascade-up, and more and more L events are generated by their own nucleation. Modified from Figure 12 in Noda et al. (2013a). (b) The number of S events normalized by the number of L events. Patch S has its characteristic earthquake if the scale ratio α is comparable to or larger than the brittleness β. Note that there is only one Patch S for one Patch L.Back to article page