Explanation for the very low Ga and Ge concentrations in some iron meteorite groups
- 1 May 1976
- journal article
- Published by Springer Nature in Nature
- Vol. 261 (5556) , 114-116
- https://doi.org/10.1038/261114a0
Abstract
No abstract availableThis publication has 13 references indexed in Scilit:
- Geochemical affinities of cobalt and germanium toward metal, silicate, and sulfide phases at high temperatureGeochimica et Cosmochimica Acta, 1974
- FRACTIONATION OF MODERATELY VOLATILE ELEMENTS IN ORDINARY CHONDRITESMeteoritics, 1974
- EMF Investigation of Ga‐Ga2O3 EquilibriumJournal of the American Ceramic Society, 1973
- Chemical fractionation in iron meteorites and its interpretationGeochimica et Cosmochimica Acta, 1972
- Thermodynamics of formation of the silicates and germanates of some divalent transition metals and of magnesiumJournal of Inorganic and Nuclear Chemistry, 1971
- Chemical fractionations in meteorites—II. Abundance patterns and their interpretationGeochimica et Cosmochimica Acta, 1967
- Chemical fractionations in meteorites—I. Condensation of the elementsGeochimica et Cosmochimica Acta, 1967
- The distribution of some trace elements in iron meteorites, as determined by neutron activationGeochimica et Cosmochimica Acta, 1967
- Tetragonal Germanium Dioxide and Equilibria in the Ge-O-H SystemJournal of the Electrochemical Society, 1965
- The Equilibrium Ge(s) + GeO2(s) = 2GeO(g). The Heat of Formation of Germanic OxideJournal of the American Chemical Society, 1952