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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Published in | Earth and planetary science letters Vol. 189; no. 1; pp. 19 - 29 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
30.06.2001
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Subjects | |
Online Access | Get full text |
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