The low‐high quartz and quartz‐coesite transition to 40 kbar between 600° and 1600°C and some reconnaissance data on the effect of NaAlO2 component on the low quartz‐coesite transition
- 10 December 1980
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 85 (B12) , 6983-6990
- https://doi.org/10.1029/jb085ib12p06983
Abstract
No abstract availableKeywords
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