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December 10, 1980Journal of Geophysical Research Atmospheres

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

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PMPeter W. MirwaldUniversität InnsbruckHMHans‐Joachim MassonneUniversity of Stuttgart

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Mirwald et al. (1980) studied this question.

synapsesocial.com/papers/6a70ac3f31a3df824328ef15https://doi.org/10.1029/jb085ib12p06983
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