Calcite-Aragonite Equilibrium at 100°C
- 26 June 1964
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 144 (3626), 1569-1570
- https://doi.org/10.1126/science.144.3626.1569
Abstract
The equilibrium pressure of the calcite-aragonite transition has been determined near 100°C and is 4.35 kilobars. These data are in agreement with earlier work but conflict with the most recent determination by Simmons and Bell.Keywords
This publication has 4 references indexed in Scilit:
- Calcite-Aragonite EquilibriumScience, 1963
- Metamorphic aragonite in the glaucophane schists of Cazadero, CaliforniaAmerican Journal of Science, 1962
- X-ray line broadening in plastically deformed calcitePhilosophical Magazine, 1959
- Phase Equilibrium in the System Calcite-AragoniteThe Journal of Chemical Physics, 1953