Experimental determination of the spinel peridotite to garnet peridotite inversion at 900° C and 1,000° C in the system CaO-MgO-Al2O3-SiO2, and at 900° C with natural garnet and olivine
- 1 January 1979
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 68 (4) , 407-419
- https://doi.org/10.1007/bf01164525
Abstract
No abstract availableKeywords
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