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Garnet porphyroblasts, containing elongate ilmenite inclusions arranged in an essentially spherical pattern, are described. The garnets are post-tectonic, and the inclusion pattern is the result of deformation and simultaneous replacement of the matrix by the growing porphyroblast.doi:10.1180/minmag.1973.039.301.13 fatcat:aowg33rk7rdfjjk6y5zcjo3tme