Metamorphic devolatilization of subducted oceanic metabasalts: implications for seismicity, arc magmatism and volatile recycling

Subducted oceanic metabasalts are believed to be a primary source of volatiles for arc magmatism and fluid-induced seismicity. From phase equilibria computed for an average oceanic metabasalt we present a model for subduction zone devolatilization for pressures up to 6 GPa (∼180 km). Along high temp...

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Bibliographic Details
Published inEarth and planetary science letters Vol. 189; no. 1; pp. 19 - 29
Main Authors Kerrick, D.M., Connolly, J.A.D.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 30.06.2001
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