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...

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Bibliographic Details
Published in:Journal of Metamorphic Geology
Main Authors: CARRINGTON, D. P., HARLEY, S. L.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1995
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1525-1314.1995.tb00246.x
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