A method for studying iron silicate liquids under reducing conditions with negligible iron loss
- 1 December 1974
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 38 (12) , 1785-1788
- https://doi.org/10.1016/0016-7037(74)90161-6
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- The join forsterite-diopside-iron oxide and its bearing on the crystallization of basaltic and ultramafic magmasAmerican Journal of Science, 1966
- Oxygen Fugacities Directly Measured in Magmatic GasesScience, 1966
- Experimental data for the system MgO-FeO-Fe 2 O 3 -CaAl 2 Si 2 O 8 -SiO 2 and their petrologic implicationsAmerican Journal of Science, 1966
- Oxygen fugacities of basaltic and andesitic magmasGeochimica et Cosmochimica Acta, 1965
- An Empirical Method for Electron Microanalysis.Analytical Chemistry, 1964
- Phase Equilibria at Liquidus Temperatures in the System MgO‐FeO‐Fe2O3‐SiO2Journal of the American Ceramic Society, 1956
- The binary systems of alumina with silica, lime, and magnesia; with optical study by Fred. Eugene WrightAmerican Journal of Science, 1909