PHASE RELATIONSHIPS IN GRANULITIC METAPELITES FROM IVREA-VERBANO ZONE (NORTHERN ITALY)
Paragneisses of the Ivrea-Verbano zone exhibit over a horizontal distance of 5 km mineralogical changes indicative of the transition from amphibolite to granulite facies metamorphism. The most obvious change is the progressive replacement of biotite by garnet via the reaction: {Mathematical expressi...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
Springer-Verlag
1976
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