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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 unit

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Submitted on : Friday, May 20, 2022 - 9:50:43 AM
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Remi Magott, Olivier Fabbri, Marc Fournier. Seismically-induced serpentine dehydration as a possible mechanism of water release in subduction zones. Insights from the Alpine Corsica pseudotachylyte-bearing Monte Maggiore ophiolitic unit. Lithos, Elsevier, 2020, 362-363, pp.105474. ⟨10.1016/j.lithos.2020.105474⟩. ⟨hal-02560403⟩

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