Since 1967 seismic source mechanism studies in the United States have seen the following major developments: 1. Detailed interpretation of fault plane solutions in terms of the new global tectonics. 2. Quantitative estimates of the rate of fault slip represented by earthquakes; interpretation of these estimates in terms of the new global tectonics; and use of such estimates to predict earthquake potential.
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James N. Brune (1971) studied this question.
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