The stability of osumilite in metapelitic granulites
Abstract A petrogenetic grid and related diagrams derived from KFMASH‐system experiments demonstrate that osumilite is stable in relatively magnesian bulk rock compositions ( X Mg > 0.6) at temperatures in excess of 875° C and pressures less than 11 kbar. The experiments, involving the dehydratio...
Published in: | Journal of Metamorphic Geology |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1995
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Subjects: | |
Online Access: | http://dx.doi.org/10.1111/j.1525-1314.1995.tb00246.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1995.tb00246.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1995.tb00246.x |