PRESSURE-TEMPERATURE DIAGRAM OF PART OF THE SIO2-H2O SYSTEM.
Abstract
The PT-projection of the high temperature part of the system SiO2-H2O is based on experimental data. The results agree with the theoretically possible scheme of combination of stable and unstable invariant points in a n = -1 multisystem according to Korzhinskii. In case of low water concentration, quartz, as a stable phase, may coexist with the melt at temperatures above 1300C. Cristobalite and tridymite are unstable at pressures higher than about 2500 atm. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Jun 01, 1966
- Accession Number
- AD0637467
Entities
People
- G. P. Mishina
- I. A. Ostrovskii
- V. M. Povilaitis
Organizations
- American Meteorological Society