INFILTRATION OF AQUEOUS FLUID AND HIGH FLUID - ROCK RATIOS DURING GREENSCHIST FACIES METAMORPHISM - A DISCUSSION
Ferry's (1984) analysis of the biotite isograd in pelitic schists of the Waterville Formation (south-central Maine, U.S.A.) led to the conclusion that metamorphism had been caused by infiltration of 1-2 rock volumes of aqueous fluid. We find that this important observation is extremely sensitiv...
| Principais autores: | , |
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| Formato: | Journal article |
| Idioma: | English |
| Publicado em: |
1986
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