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catalogo de terremotos para america del sur catalog of earthquakes ...

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Shallow: 0-70 kms.<br />

S11<br />

Intermediate: 70-300 kms.<br />

Deep: Greater than 300 kms.<br />

The second plot groupEd the events into two magnitu<strong>de</strong> ranges: one with<br />

6.5 > M s < 8.0, and the second with magnitu<strong>de</strong>s > 8.0. Events with magnitu<strong>de</strong>s<br />

> 8.0 are labeled by year <strong>of</strong> occurrence. In or<strong>de</strong>r to divi<strong>de</strong> the events into<br />

rajiges based on M. magnitu<strong>de</strong>s, it was necessary to compute an M. magnitu<strong>de</strong> for<br />

events which iad only an mb magnitu<strong>de</strong> reported or only a maximum intensity. A<br />

least squares regression was done, regressing Ms on mb using the <strong>catalog</strong> data<br />

for events <strong>of</strong> a <strong>de</strong>pth less than or equal to 55 kms. The value <strong>of</strong> 55 kms was<br />

selected as the cut<strong>of</strong>f for shallow events after a qualitative examination <strong>of</strong><br />

the distribution <strong>of</strong> <strong>de</strong>pths in the <strong>catalog</strong>. This regression produced the<br />

following formula:<br />

M s = -6.411 + 2.18 mb (1)<br />

This formuia was used to compute an Ms value if there was no M. value but an<br />

mb value was available. A second regression was done regressing Ms on Io,<br />

also for events with a <strong>de</strong>pth less than or equal to 55 kms. This regression<br />

produced the following equation:<br />

M s = 1.26 + 0.63 I o<br />

This is very similar to the equation <strong>de</strong>rived by Gutenberg and Richter (1956)<br />

which is:<br />

M = 1 + 2/3 I o<br />

Equation 2 was used to compute Ms from Io if no magnitu<strong>de</strong> values were<br />

available. In Chile, estimated values <strong>of</strong> Ms (listed un<strong>de</strong>r other magnitu<strong>de</strong>s)<br />

(3)<br />

(2)

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