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Un evento de deslizamiento silencioso en la interfaz de subducción más profunda de Cascadia.

G Dragert1, K Wang, T S James

  • 1Geological Survey of Canada, Pacific Geoscience Centre, 9860 West Saanich Road, Sidney, British Columbia, Canada V8L 4B2. dragert@pgc.nrcan.gc.ca

Science (New York, N.Y.)
|April 21, 2001
PubMed
Resumen

Los datos del Sistema de Posicionamiento Global continuo revelaron movimiento hacia tierra en Columbia Británica y Washington debido a la falla de subducción de Cascadia bloqueada. Un evento de 1999 mostró un deslizamiento sísmico, lo que indica pulsos discretos de movimiento en la interfaz de falla.

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