Scaling relations among seismic moment, M-0, average displacement, del
ta rupture width, W and rupture length, L, of earthquake faults are st
udied mainly using the data base of earthquake source parameters compi
led by Wells and Coppersmith (1994). Results show that seismic moment
scales with rupture length approximately as M-0 - L-2; rupture width i
s independent of rupture length for large earthquakes; average displac
ement relates to rupture length approximately as delta - L; and the av
erage displacement is independent of rupture width. Consequently,the L
-model proposed by Scholz (1982) is more appropriate than the W-model
suggested by Romanowicz (1992) to describe the scaling of earthquake f
aults.