Stress drop and frictional heating during the 1994 Deep Bolivia Earthquake

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Frictional melting during the rupture of the 1994 bolivian earthquake

The source parameters of the 1994 Bolivian earthquake (magnitude Mw = 8.3) suggest that the maximum seismic efficiency eta was 0.036 and the minimum frictional stress was 550 bars. Thus, the source process was dissipative, which is consistent with the observed slow rupture speed, only 20% of the local S-wave velocity. The amount of nonradiated energy produced during the Bolivian rupture was com...

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 1999

ISSN: 0094-8276

DOI: 10.1029/1999gl005410