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Record of intermediate-depth subduction seismicity in a dry slab from an exhumed ophioliteG. Pennacchioni, M. Scambelluri, M. Bestmann, et al.
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Seismically-induced serpentine dehydration as a possible mechanism of water release in subduction zones. Insights from the Alpine Corsica pseudotachylyte-bearing Monte Maggiore ophiolitic unitRémi Magott, Olivier Fabbri and Marc Fournier
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