The dependence of the summed moment release on the fault dimension dif
fers between non-creeping faults and creeping faults or volcanic regio
ns. This can be attributed to different earthquake scaling laws. The n
umber N of events with fault length L scales for non-creeping faults a
s N(L)similar to L(-2) and for creeping faults as N(L)similar to L(-3)
. This difference offers a means for mapping the distribution of creep
in the seismogenic crust.