Osumilite-sapphirine-quartz granulites from Enderby Land, Antarctica: P-T conditions of metamorphism, implications for garnet-cordierite equilibria and the evolution of the deep crust
- 1 January 1980
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 74 (2) , 201-210
- https://doi.org/10.1007/bf01132005
Abstract
No abstract availableKeywords
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