Experimental and natural partitioning of Th, U, Pb and other trace elements between garnet, clinopyroxene and basaltic melts
- 1 November 1994
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 117 (1-4) , 149-166
- https://doi.org/10.1016/0009-2541(94)90126-0
Abstract
No abstract availableKeywords
This publication has 43 references indexed in Scilit:
- Experimental rare earth element partition coefficients for garnet, clinopyroxene and amphibole coexisting with andesitic and basaltic liquidsPublished by Elsevier ,2003
- Experimental determination of U and Th partitioning between clinopyroxene and natural and synthetic basaltic liquidPublished by Elsevier ,2002
- Closure temperatures of the Sm—Nd system in metamorphic garnetsPublished by Elsevier ,2002
- Sr, Nd, and Pb isotopes of ultramafic xenoliths in volcanic rocks of Eastern China: enriched components EMI and EMII in subcontinental lithospherePublished by Elsevier ,2002
- Thorium-Uranium Fractionation by Garnet: Evidence for a Deep Source and Rapid Rise of Oceanic BasaltsScience, 1993
- The generation of uranium series disequilibria by partial melting of spinel peridotite: constraints from partitioning studiesEarth and Planetary Science Letters, 1993
- Dynamic disequilibrium melting model with porous flow and diffusion-controlled chemical equilibrationEarth and Planetary Science Letters, 1993
- Nd and Sr isotopic study of a mafic layer from Ronda ultramafic complexNature, 1983
- The partitioning of rare earth elements between garnet and liquid at high pressures: Preliminary experimentsGeophysical Research Letters, 1975
- Correction factors for electron probe microanalysis of silicates, oxides, carbonates, phosphates, and sulfatesAnalytical Chemistry, 1970