The quartz-coesite transition
- 1 February 1960
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 65 (2), 749-756
- https://doi.org/10.1029/jz065i002p00749
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Apparatus for phase-equilibrium measurements at pressures up to 50 kilobars and temperatures up to 1750°CJournal of Geophysical Research, 1960
- The crystal structure of coesite, the dense, high-pressure form of silicaZeitschrift für Kristallographie, 1959
- Experimental determination of kyanite-sillimanite equilibrium relations at high temperatures and pressuresAmerican Journal of Science, 1957
- Quartz-coesite stability relations at high temperatures and pressuresAmerican Journal of Science, 1956
- A simple apparatus for high pressures and temperaturesAmerican Journal of Science, 1956
- A New Dense Crystalline SilicaScience, 1953
- Change of Melting Point of Diopside with PressureThe Journal of Geology, 1952
- High‐low quartz inversion up to 10,000 barsEOS, Transactions American Geophysical Union, 1950
- Thermodynamic Properties of the Crystalline Forms of SilicaJournal of the American Chemical Society, 1941
- Explorations toward the Limit of Utilizable PressuresJournal of Applied Physics, 1941