Abstract: MnO zoning profiles for various sizes of garnets from two pelitic schists were examined. The data from garnets of specimen A are consistent with a constant growth law, while the compositional-crystal size relationships of garnets from specimen B are best explained by heterogeneous growth rates.
Mineralogical Magazine; October 1987 v. 51; no. 62; p. 569-576; DOI: 10.1180/minmag.1987.051.362.11
© 1987, The Mineralogical Society
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