The composition of melt inclusions in minerals at the garnet-spinel transition zone

High-pressure melts are preserved as inclusions in automorphous spinel crys tals from reaction coronas surrounding pyrope garnets in lherzolites from L ashaine volcano, northern Tanzania. The inclusions are primary; i.e, they c ontain liquids that have formed in thermodynamic equilibrium with their hos t spinels and the trapping pressures of the melts correspond to those of th e host spinel growths. Calibrations of the spinel-garnet phase equilibrium transition suggest that the spinel containing the melt inclusions formed at pressures around 2.5 GPa, and mass balance calculations indicate that the inclusions contain melts formed by low-degree of melting (F approximate to 0.04) during garnet breakdown. Despite the possibility that full equilibrat ion was not attained with all the mineral phases found in the nodules, the melt inclusions, after homogenization by high-T experiments, display compos itions remarkably consistent with experimental melts obtained at pressures around 2.5 GPa on natural and model peridotite systems. They are characteri zed by lower SiO2 (47.5 wt% on average) and higher MgO and FeO contents, at a given Na2O+K2O content, than low-degree melt inclusions formed around 1. 0 GPa and preserved in spinel-peridotite minerals. This provides direct evi dence for the hypothesis that for low-degree melts, the decrease in SiO2 wi th pressure is superimposed on a decrease of the effect of alkali oxides on the silica activity coefficient, thereby generating melts with a compositi on more akin to erupted alkali basalt than at shallow depths, (C) 2000 Else vier Science B.V. All rights reserved.