Olivine/silicate melt partitioning of germanium: an example of a nearly constant partition coefficient
- 1 February 1982
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 46 (2) , 235-240
- https://doi.org/10.1016/0016-7037(82)90250-2
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Partitioning of Ni between olivine and silicate melt: The ‘Henry's Law problem’ reexaminedGeochimica et Cosmochimica Acta, 1981
- GeSi and GaAl fractionation in Hawaiian volcanic rocksGeochimica et Cosmochimica Acta, 1978
- A review of experimental studies of crystal/liquid trace element partitioningGeochimica et Cosmochimica Acta, 1978
- Partition of Sr, Ba, Ca, Y, Eu2+, Eu3+, and other REE between plagioclase feldspar and magmatic liquid: an experimental studyGeochimica et Cosmochimica Acta, 1975
- Kinetic disequilibrium in trace element partitioning between phenocrysts and host lavaGeochimica et Cosmochimica Acta, 1972
- Zur geochemie des germaniumsGeochimica et Cosmochimica Acta, 1963
- High pressure studies of the system Mg 2 GeO 4 Mg 2 SiO 4 with special reference to the olivine-spinel traansitionAmerican Journal of Science, 1960
- The abundances of gallium and germanium in terrestrial materialsGeochimica et Cosmochimica Acta, 1959
- On the geochemistry of germaniumGeochimica et Cosmochimica Acta, 1957
- The distribution of germanium among coexisting phases of partly glassy rocksGeochimica et Cosmochimica Acta, 1954