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DEPARTMENTO DE GEOFÍSICA INSTITUTO ASTRONÔMICO E GEOFÍSICO UNIVERSIDADE DE SÃO PAULO, P.O. BOX 30627, SÃO PAULO, SP, Brazil
Abstract
An empirical amplitude-distance curve is determined for earthquakes registered at regional distances in conterminous Brazil. This curve is the basis of a regional magnitude scale, mR, using the maximum amplitude in the whole P-wave train with periods in the range 0.1 to 1.0 sec. In the distance range 200
R
1500 km, we find
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This scale gives much better agreement with the teleseismic mb magnitudes than the values calculated using the regional Q factors of Gutenberg and Richter (1956). It is shown that, despite using a wide range of periods, mR should be a good estimate of the 1-sec teleseismic mb in the range 2
mb < 5.
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