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The fault parameters of the Guam earthquake of August 8, 1993 are estimated from seismological analyses, and the possibility of identifying the actual fault plane from tsunami waveforms is tested. The Centroid Moment Tensor solution of long-period surface waves shows one nodal plane shallowly dipping to the north and the other nodal plane steeply dipping to the south. The seismic moment is 3.5×10 20 Nm and the corresponding moment magnitude is 7.7. The Moment Tensor Rate Function inversion of P waves also yields a similar focal mechanism and seismic moment. The point source depth is estimated as 40–50 km

Analysis of seismological and tsunami data from the 1993 Guam earthquake