Pressure, temperature and C-O-H fluid fugacities across the amphibolite-granulite transition, Northwest adirondack mountains, New York

Keyphrases

• Garnet 100%
• Pressure-temperature 100%
• Granulite 100%
• Amphibolite 100%
• Fugacity 100%
• Biotite 100%
• Adirondack Mountains 100%
• C-O-H Fluid 100%
• Feldspar 66%
• Non-ideality 66%
• Silica 33%
• Rutile 33%
• Partial Melting 33%
• Increased Temperature 33%
• Water Activity 33%
• Graphite 33%
• Muscovite 33%
• Metamorphism 33%
• Dehydration Reaction 33%
• Anorthite 33%
• Granulite Facies 33%
• Temperature Water 33%
• Sillimanite 33%
• High-grade Metamorphism 33%
• Zoning Patterns 33%
• Adirondacks 33%
• Grossular 33%
• Almandine 33%
• Minimum Pressure Drop 33%
• Compositional Zoning 33%
• Paragneiss 33%
• Pyrope 33%
• Barometry 33%
• Fluid Species 33%

Earth and Planetary Sciences

• Peridotite 100%
• Garnet 100%
• Fugacity 100%
• Amphibolite 100%
• Granulite 100%
• Carbon Dioxide 66%
• Partial Melting 33%
• Water Temperature 33%
• Locale 33%
• Granulite Facies 33%
• Sillimanite 33%
• Almandine 33%
• Pyrope 33%
• Grossular 33%
• Barometry 33%
• Muscovite 33%