The Archean granulite-facies rocks of the northern Wind River Range consist of extensive granitic orthogneisses and migmatites hosting banded iron formations, amphibolites, metapelites, metabasites, ultramafites and quartzites. Quantitative pressure and temperature estimates from inclusions within garnet porphyroblasts are 815±5O%C and 8±1 kb using equilibria buffered by the assemblages spinel-quartz-garnet-sillimanite and garnet-rutile-ilmenite-sillimanite-quartz. Pressure-temperature estimates from the groundmass core assemblages of the banded iron formations and hornblende granulites are 750 ±50 %C and 5·5 ± 1 kb using garnet-clinopyroxene, garnet-orthopyroxene, and two-pyroxene thermometry, and geobarometers based on the assemblages garnet-quartz-plagioclase-orthopyroxene and orthopyroxene-olivine-quartz. Rim compositions of the matrix minerals indicate nearly isobaric cooling from the conditions of 750 %C and 5-5 kb to < 600%C at 5 kb. Taken together, the P-T estimates from both the garnet inclusions and matrix assemblages are consistent with a clockwise P-T-t path for this terrane. Temperature estimates based on oxygen isotope thermometry in the banded iron formations vary systematically with the degree of visible late-stage deformation. There is no correlation between the isotopic temperature estimates and those from cation-based thermometers. The highest pressures and temperatures for the Wind River terrane are preserved by the inclusions in garnet porphyroblasts. The ability of these inclusions to preserve chemistries corresponding to higher pressures and temperatures is attributed to the combined effects of inclusion isolation and fixed inclusion volume within the garnet porphyroblasts. Cation-based thermometers in the groundmass preserve lower temperatures as a result of diffusional partial resetting. Isotopic thermometry will yield the lowest temperatures if there is even minor retrograde deformation. Geothermobarometry for the northern Wind River Archean terrane is consistent with a tectonic regime of doubly thickened crust. Peak metamorphic conditions preserved in the cores of the garnets are compatible with deep burial during the early stages of tectonism. Rapid to intermediate uplift due to erosion of the upper plate could explain the nearly isothermal decompression from 8·0 to 5-5 kb. The later, nearly isobaric, cooling path indicated by the rim compositions of the matrix minerals is consistent with relaxation of the elevated geother
