Statistical analysis of stress drops in Mexico with an application to accelerations of the ground
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El análisis estadístico de caídas de esfuerzo, p, de 5 grupos de temblores en California y México confirma que la distribución de densidad de p es proporcional a p-l+α(α <0). El resultado había sido predicho por Caputo (1976). La distribución de densidad de p nos permite computar el período de retorno de aceleraciones del suelo (Caputo, 193la) y encontrar signos precursores de temblores (Caputo, 1981 b).
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