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Updated: Jul 12, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

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La estabilidad de la serpentina a las profundidades del manto y el magmatismo relacionado con la subducción

P Ulmer, V Trommsdorff

    Science (New York, N.Y.)
    |May 12, 1995
    PubMed
    Resumen

    Los experimentos de alta presión revelan que la descomposición de la antigorita en las rocas hidratadas del manto libera agua significativa. Esta agua puede desencadenar una fusión parcial, formando magmas calc-alcalinos en las zonas de subducción.

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