THE STABILITY OF OSUMILITE IN METAPELITIC GRANULITES

A petrogenetic grid and related diagrams derived from KFMASH-system experiments demonstrate that osumilite is stable in relatively magnesian bulk rock compositions (X(Mg) > 0.6) at temperatures in excess of 875 degrees C and pressures less than 11 kbar. The experiments, involving the dehydration melting of biotite in synthetic metapelites, were conducted in the range 850-1000 degrees C. Both the mineral assemblages and phase compositions reported from well-documented natural examples of osumilite-bearing rocks are reproduced by the experiments at P-T conditions similar to those previously estimated for these occurrences. Peak metamorphic P-T conditions can be reliably inferred from distinctive osumilite-bearing assemblages identified in the phase diagrams, thereby avoiding the problems of diffusional re-equilibration that often prohibits conventional geothermobarometry from recovering peak conditions. Integration of the experimental data with recent independent experiments, after correcting the latter for an underestimated friction correction, allows extension of the petrogenetic grid to higher temperatures. The extended grid is applied to assess and refine the metamorphic history of the Napier Complex, East Antarctica: the high-P stability limit for osumilite in the Napier Complex is 9-10 kbar, the prograde P-T-t path is not necessarily anticlockwise and isobaric cooling in the Scott and Tula mountains occurred, respectively, at pressures greater and Less than reactions in the range 8-9 kbar. The stability range for osumilite predicted by the KFMASH-system petrogenetic grid overlaps many more metamorphic terranes than osumilite is found in. Whilst osumilite is not distinctive in thin section and is prone to retrogression, it is possible that carbon dioxide present in the natural system stabilizes cordierite at the expense of osumilite.