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- W59112413 abstract "A unique garnetiferous occurrence of Proterozoic mafic rocks in the south-central Llano Uplift near Oxford in central Texas provides evidence supporting the hypothesis that rocks in the southeast uplift shared the high-pressure metamorphism recorded in remnants of mafic eclogites in the northwest uplift (Mason County eclogite: Wilkerson et al., 1988) and northern uplift (Whitt Ranch metagabbro: Schwarze, 1990). Petrologic features that formed during early high-pressure metamorphism have been partly obscured, however, by late amphibolite-facies retrogression at low pressure, which overprinted many rocks throughout the uplift. Prior to this study of the Oxford body, involvement of the rocks in the southeast portion of the uplift in an early high-pressure metamorphic event had been inferred only on the basis of staurolite textures and chemistry from two localities in the Precambrian Rough Ridge Formation and from regional trends in homogenization of prograde garnet zoning (Carlson and Nelis, 1986; Carlson and Schwarze, 1993; Carlson and Reese, 1994)." @default.
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- W59112413 date "1998-01-01" @default.
- W59112413 modified "2023-09-26" @default.
- W59112413 title "Proterozoic Evolution of the Llano Uplift, Central Texas: Evidence for High-Pressure Metamorphism from the Oxford Mafic Body" @default.
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- W59112413 doi "https://doi.org/10.1007/978-94-011-5098-9_19" @default.
- W59112413 hasPublicationYear "1998" @default.
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