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

Remi Magott (1) , Olivier Fabbri (1) , Marc Fournier (2)

1 LCE - Laboratoire Chrono-environnement (UMR 6249)
2 iSTeP - Institut des Sciences de la Terre de Paris

Domaines: Tectonique

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, 2020, 362-363, pp.105474. ⟨10.1016/j.lithos.2020.105474⟩. ⟨hal-02560403⟩