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Zona de falla del manto debajo del volcán Kilauea, Hawai

Cecily J Wolfe1, Paul G Okubo, Peter M Shearer

  • 1Hawaii Institute of Geophysics and Planetology, University of Hawaii at Manoa, Honolulu, HI96822, USA. wolfe@hawaii.edu

Science (New York, N.Y.)
|April 19, 2003
PubMed
Resumen

Los terremotos profundos en el volcán Kilauea se originan por fallas tectónicas, no por magma. La sismicidad revela el deslizamiento hacia el mar en un plano de falla de ángulo bajo a 30 kilómetros de profundidad, lo que indica estrés litosférico.

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