The system CaO-MgO-FeO-SiO2 and its bearing on the origin of ultrabasic and basic rocks
- 1 June 1960
- journal article
- Published by Mineralogical Society in Mineralogical Magazine and Journal of the Mineralogical Society
- Vol. 32 (249), 459-470
- https://doi.org/10.1180/minmag.1960.032.249.05
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
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- A chemical definition of fractionation stages as a basis for comparison of Hawaiian, Hebridean and other basic lavasGeochimica et Cosmochimica Acta, 1956
- Some basaltic provincesGeochimica et Cosmochimica Acta, 1955
- Composition and origin of basaltic magma of the Hawaiian IslandsGeochimica et Cosmochimica Acta, 1955
- THE SYSTEM MgO—SiO2—H2OGSA Bulletin, 1949
- A primary peridotite magmaAmerican Journal of Science, 1938
- The system MgO-FeO-SiO 2American Journal of Science, 1935
- Trends of differentiation in basaltic magmasAmerican Journal of Science, 1933
- The Physical Chemistry of the Crystallization and Magmatic Differentiation of Igneous RocksThe Journal of Geology, 1922