Publication | Open Access

Fluid-related inclusions in Alpine high-pressure peridotite reveal trace element recycling during subduction-zone dehydration of serpentinized mantle (Cima di Gagnone, Swiss Alps)

EngineeringFluid-related InclusionsIgneous PetrogenesisGeologyGeochemistrySubduction-zone DehydrationPetrologySwiss AlpsMantle GeochemistryTectonics