EXPERIMENTAL-STUDY OF THE SYSTEM PHLOGOPITE-DIOPSIDE FROM 3.5 TO 17 GPA

On the basis of both natural samples and experimental studies, clinopy roxene is a potential reservoir for potassium in the Earth's mantle. T he amount of K partitioning into clinopyroxene depends on the phase as semblage present, the bulk composition, pressure, and temperature. To investigate some of these dependencies, subsolidus and melting phase r elations in the system phlogopite-diopside have been studied to 17 Cpa . In this system, phlogopite becomes unstable with increasing pressure , breaking down to potassium richterite, which in turn breaks down to another K-bearing hydrous phase (phase X), such that a K-rich phase co exists with clinopyroxene to 17 Cpa. Clinopyroxenes contain less than or equal to 1.3 wt% K2O in assemblages of phlogopite + clinopyroxene /- olivine +/- liquid at 3-5 Gpa, phlogopite + clinopyroxene + garnet +/- olivine +/- liquid at 7-9 GPa, clinopyroxene + garnet + olivine +/ - potassium richterite +/- liquid at 11 Gpa, and clinopyroxene + olivi ne + garnet + phase X at 14 and 17 GPa. In these assemblages, K is par titioned into hydrous phases or liquid, rather than into the clinopyro xene. By inference, phlogopite (or its higher-pressure breakdown produ cts) is the primary host for K in the mantle (if H2O is present), and any coexisting clinopyroxene has very low concentrations of K. Convers ely, the natural occurrence of clinopyroxene with >> 1 wt% K2O require s that phlogopite, potassium richterite, or phase X is not stable in t he local source environment of such samples.