[HTML][HTML] Dating fluid infiltration and deformation in the subducted ultramafic oceanic lithosphere by perovskite geochronology
Carbonated ultramafic rocks (ie, ophicarbonates) form by peridotite serpentinization and
carbonation at the seafloor. Their metamorphic evolution is linked to that of serpentinites …
carbonation at the seafloor. Their metamorphic evolution is linked to that of serpentinites …
Global Hydrogen Production During High‐Pressure Serpentinization of Subducting Slabs
Serpentinization is among the most important, and ubiquitous, geological processes in
crustal–upper mantle conditions (< 6 GPa,< 600° C), altering the rheology of rocks and …
crustal–upper mantle conditions (< 6 GPa,< 600° C), altering the rheology of rocks and …