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Despite the widespread presence of hydrous phases in subduction- related systems, experimental DMin/Fluid trace element values for many hydrous phases are lacking. To fill this gap, we present a set of DMin/Clinopyroxene values (where Min indicates amphibole, zoisite, phengite, paragonite or apatite) derived from equilibrium parageneses of eclogites from Trescolmen (Central Alps, Switzerland). The...

Equilibrium and Disequilibrium Trace Element Partitioning in Hydrous Eclogites (Trescolmen, Central Alps)