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Published on: August 7, 2017

Evolución del temblor no volcánico y los terremotos de San Simeon y Parkfield, California

Robert M Nadeau1, Aurélie Guilhem

  • 1Berkeley Seismological Laboratory, University of California, Berkeley, CA 94720, USA.

Science (New York, N.Y.)
|July 11, 2009
PubMed
Resumen

Los temblores no volcánicos cerca de fallas bloqueadas pueden preceder a los terremotos. Después de dos grandes terremotos, la actividad de temblores en la Falla de San Andrés se mantuvo elevada durante años, lo que indica un estrés acumulado.

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