Experimental chlorine partitioning between forsterite, enstatite and aqueous fluid at upper mantle conditions

Cl partition coefficients between forsterite, enstatite and coexisting Cl-bearing aqueous fluids were determined in a series of high pressure and temperature piston cylinder experiments at 2GPa between 900 and 1300°C in the system MgO–SiO2–H2O–NaCl–BaO–C±CaCl2±TiO2±Al2O3±F. Diamond aggregates were a...

Ausführliche Beschreibung