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Large earthquakes within stable continen-3 tal regions (SCR) show that significant amounts 4 of elastic strain can be released on geological 5 structures far from plate boundary faults, where 6 the vast majority of the Earth's seismic ac-7 tivity takes place. SCR earthquakes show spa-8 tial and temporal patterns that differ from those 9 at plate boundaries and occur in regions where 10 tectonic loading rates are negligible. However, 11 in the absence of a more appropriate model, 12 they aredoi:10.1130/abs/2017am-303722 fatcat:vom2vbaxifgc3j6lwwjvsnqxsu