Metastability of an osumilite end member in the system K2O-MgO-Al2O3-SiO2-H2O and its possible bearing on the rarity of natural osumilites
- 1 May 1967
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 14 (4) , 343-358
- https://doi.org/10.1007/bf00373812
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- Die Genese der metamorphen GesteinePublished by Springer Nature ,1965
- Metastable solid solutions with quartz-type structures on the join SiO2–MgAl2O4Zeitschrift für Kristallographie, 1961
- Hydrothermale und röntgenographische Untersuchungen an gesteinsbildenden Mineralen—V: Über hydrothermal hergestellen OsumilithGeochimica et Cosmochimica Acta, 1958
- The System K2O‐MgO‐AI2O3‐SiO2: I, Results of Quenching Experiments on Four Joins in the Tetrahedron Cordierite‐forsterite‐leucite‐Silica and on the Join Cordierite‐Mullite‐Potash FeldsparJournal of the American Ceramic Society, 1954
- Osumilite, a New Mineral, and Cordierite in Volcanic RocksProceedings of the Japan Academy, 1953
- The crystal structure of milariteActa Crystallographica, 1952
- The system K 2 O-MgO-SiO 2 ; Part 1American Journal of Science, 1951