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We examined how the relationships systematically change among the moment magnitude MW, the Japan Meteorological Agency magnitude MJ, and the short-period magnitude m for inland earthquakes classified by fault type. The examination was extended to the relationships among the magnitudes for inter-plate earthquakes and to those for slab earthquakes. It was found out that MJ was about 0.5 larger than MW in inland earthquakes caused by strike-slip faults, MJ was about 0.2 larger than MW in inland earthquakes caused by dip-slip faults, m was about 0.2 smaller than MW in inland earthquakes caused by strike-slip faults, and m was about 0.1 larger than MW in inland earthquakes caused by dip-slip faults. We applied these relationships to the procedure for evaluating fault parameters, and showed two examples of strong motions predicted for strike-slip and dip-slip faults 40 km long.

RELATIONSHIPS AMONG DIFFERENT MAGNITUDES FOR INLAND EARTHQUAKES CLASSIFIED BY FAULT TYPE AND THEIR APPLICATION TO STRONG MOTION PREDICTION