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Los temblores no volcánicos y los terremotos de baja frecuencia hacen enjambres

David R Shelly1, Gregory C Beroza, Satoshi Ide

  • 1Department of Geophysics, 397 Panama Mall, Stanford University, Stanford, California 94305-2215, USA. dshelly@pangea.stanford.edu

Nature
|March 16, 2007
PubMed
Resumen

El temblor no volcánico, una señal sísmica cerca de fallas, se explica como numerosos pequeños terremotos. Este hallazgo sugiere que los eventos de temblor y deslizamiento lento son fenómenos vinculados, que ofrecen información sobre los procesos de falla y el peligro sísmico.

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