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Updated: Jul 12, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

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El papel de los cambios de fase a poca profundidad en la subducción de la corteza oceánica

W D Pennington

    Science (New York, N.Y.)
    |June 3, 1983
    PubMed
    Resumen

    Las placas tectónicas subductoras cambian de ángulo a 40 km de profundidad debido a los cambios de fase en la corteza oceánica. Estos cambios de fase también pueden causar terremotos en la zona superior de Benioff.

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