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- W2168855276 abstract "Late Archean and Early Proterozoic continental margin pelites, graywackes, and quartzites in today.s Black Hills were regionally metamorphosed during the collision of the Archean Wyoming and Superior provinces beginning at ~1755 Ma. During east-west regional compression, metamorphism reached incipient garnet-biotite grade conditions at ~400 °C. Unzoned garnet (Sps44Alm44Pyr3Grs9) characterizes the mineral assemblage in graphitic metapelites. The low-temperature onset of the garnet-biotite assemblage is attributed to high Mn concentrations and low aH₂O due to the presence of CH4 and CO2." @default.
- W2168855276 created "2016-06-24" @default.
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- W2168855276 date "2006-10-01" @default.
- W2168855276 modified "2023-10-03" @default.
- W2168855276 title "Fluid-mediated polymetamorphism related to Proterozoic collision of Archean Wyoming and Superior provinces in the Black Hills, South Dakota" @default.
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- W2168855276 doi "https://doi.org/10.2138/am.2006.2120" @default.
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