The miscibility of the pyralspite and grandite molecules in garnets
- 1 September 1967
- journal article
- Published by Mineralogical Society in Mineralogical Magazine and Journal of the Mineralogical Society
- Vol. 36 (279), 389-402
- https://doi.org/10.1180/minmag.1967.036.279.09
Abstract
SummaryThough the transitional members between the pyralspite and grandite series occur only very sporadically, there exists under favourable conditions a perfect miscibility between grossular on the one hand, and spessartine or almandine or pyrope on the other. The conditions favouring this miscibility are discussed.Keywords
This publication has 13 references indexed in Scilit:
- Petrogenesis of Franciscan glaucophane schists and associated metamorphic rocks, CaliforniaContributions to Mineralogy and Petrology, 1965
- Note on a chrome and two manganese garnets from IndiaMineralogical Magazine and Journal of the Mineralogical Society, 1963
- Garnet Types from the Cazadero Area, CaliforniaJournal of Petrology, 1963
- Glaucophane-bearing Metamorphic Rock Types of the Cazadero Area, CaliforniaJournal of Petrology, 1963
- The join Ca 3 Al 2 Si 3 O 12 -Mg 3 Al 2 Si 3 O 12 and its bearing on the system CaO-MgO-Al 2 O 3 -SiO 2 at atmospheric pressureAmerican Journal of Science, 1962
- Zur Kristallehemie der GranateContributions to Mineralogy and Petrology, 1962
- METAMORPHIC REACTIONS AND METAMORPHIC FACIESPublished by Geological Society of America ,1958
- High‐pressure MineralsJournal of the American Ceramic Society, 1955
- Studier över Yxsjöfältets geologi och petrografiGeologiska Föreningen i Stockholm Förhandlingar, 1922
- Om granatens natur uti de mellansvenska malmfyndig-heternas skarnbildningarGeologiska Föreningen i Stockholm Förhandlingar, 1919