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- W1872819868 abstract "Observed maximum rotation (Ωe) of schistosity and compositional banding (fiducial surface) encapsulated in and passing through the center of a garnet relative to the same surface away from the garnet (fiducial plane = S) commonly results from a sequence of velocity gradients ([∂u̇ i /∂x j ] or [u̇ i , j ]) that have affected the surrounding rock. The circumstances under which Ωe represents the cumulative rotational motion, ∫ ω̇dt = Ω, resulting from the antisymmetric part of [u̇ i , j ] are described, assuming the garnet to have..." @default.
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- W1872819868 date "1970-01-01" @default.
- W1872819868 modified "2023-10-06" @default.
- W1872819868 title "Rotated Garnets in Metamorphic Rocks" @default.
- W1872819868 doi "https://doi.org/10.1130/spe129-p1" @default.
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