CO2-rich Fluid Inclusions in Greenschists, Migmatites Granulites, and Hydrated Granulites
Abstract
Data was discussed from several different terrains in which CO2-rich fluid inclusions occur despite parageneses that predict the presence of H2O-rich fluids. CO2-rich fluid inclusions, some having densities appropriate for peak-metamorphic conditions, were found in greenschists, amphibolites, migmatites, and hydrated granulites. The author suggested that there may be a common process that leads to CO2-rich secondary inclusions in metamorphic rocks.
- Publication:
-
Workshop on the Deep Continental Crust of South India
- Pub Date:
- 1988
- Bibcode:
- 1988dcc..work...70H
- Keywords:
-
- Granite;
- Inclusions;
- Metamorphism (Geology);
- Petrology;
- Schist;
- Carbon Dioxide Concentration;
- Gneiss;
- Terrain;
- Geophysics