Surface-wave magnitudes (M(8)) of 4.1 and 3.2 are determined for two events in southern Algeria. The corresponding body-wave magnitudes (m(b)) are 5.8 and 4.9, respectively. The surface waves from these events are much smaller than would be expected from most earthquakes of comparable body-wave magnitudes, which fact suggests that these waves were generated by underground explosions.
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Liebermann et al. (1967) studied this question.
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