Near mantle solidus trace element partitioning at pressures up to 3.4 GPa
Author:
Affiliation:
1. National High Magnetic Field Laboratory and Department of Geological Sciences; 1800 E. Paul Dirac Drive, Tallahassee Florida 32306 USA
2. Lamont-Doherty Earth Observatory of Columbia University; Rte 9W, Palisades New York 10964 USA
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Reference72 articles.
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3. Determining the composition of high-pressure mantle melts using diamond agregates;Baker;Geochim. Cosmochim. Acta,1994
4. The generation of uranium series disequilibria by partial melting of spinel peridotite: Constraints from partitioning studies;Beattie;Earth Planet. Sci. Lett.,1993
5. Uranium-thorium disequilibria and partitioning on melting of garnet peridotite;Beattie;Nature,1993
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