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- W2135910963 abstract "Marbles and metapelites from the Reynolds Range Group (central Australia) were regionally metamorphosed at low pressure during M2 at ∼1.6 Ga, M2 ranged in grade from greenschist to granulite facies along the length of the Reynolds Range, and overprinted ∼1.78 Ga granites and their contact aureoles in the Reynolds Range Group metasediments. At all M2 grades the marbles and metapelites have highly variable oxygen isotope ratios [marbles: δ18O(carb) ∼ 14–20%‰; metapelites: δ18O ∼ 6–14%‰). Similarly, ∼ 1.78 Ga granites have highly variable oxygen isotope ratios (δ18O ∼ 5–13%‰), with the lowest values occurring at the granite margins. In all rock types, the lowest oxygen isotope values are consistent with the infiltration of channelled magmatic and/or meteoric fluids. The variable lowering of oxygen isotope values resulted from pre-M2 contact metamorphism and fluid—rock interaction around the ∼1.78 Ga granites. In contrast, mineral assemblages in the marbles define a trend of increasing XCO2 with increasing grade from <0.05 (greenschist facies) to ∼0.7–1.0 (granulite facies). This, together with the lack of regionally systematic resetting of oxygen isotope ratios, implies that there was little fluid—rock interaction during prograde regional metamorphism." @default.
- W2135910963 created "2016-06-24" @default.
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- W2135910963 date "1996-01-01" @default.
- W2135910963 modified "2023-10-01" @default.
- W2135910963 title "Fluid—Rock Interaction during Low-Pressure Polymetamorphism of the Reynolds Range Group, Central Australia" @default.
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- W2135910963 doi "https://doi.org/10.1093/petrology/37.5.1097" @default.
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