Abstract
The effect of total solution concentration on the Ca: Mg ratio at the magnesitedolomite and the dolomite-calcite boundaries in CaCl2MgCl2CO2 solutions has been determined between 280 and 420°C. Below about 410° a decrease in the total concentration of the solutions produces a displacement of both boundaries toward lower values of the Ca:Mg ratio. Observed displacements are small but increase with decreasing temperature.
Original language | English (US) |
---|---|
Pages (from-to) | 391-396 |
Number of pages | 6 |
Journal | Geochimica et Cosmochimica Acta |
Volume | 31 |
Issue number | 3 |
DOIs | |
State | Published - Mar 1967 |
Externally published | Yes |
ASJC Scopus subject areas
- Geochemistry and Petrology