U-series isotope evidence for the origin of continental basalts
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference39 articles.
1. Experimental determination of U and Th partitioning between clinopyroxene and natural and synthetic basaltic liquid;LaTourrette;Earth Planet. Sci. Lett.,1992
2. Thorium-uranium fractionation by garnet: Evidence for a deep source and rapid rise of oceanic basalts;LaTourrette;Science,1993
3. Uranium-thorium disequilibria and partitioning on melting of garnet peridotite;Beattie;Nature,1993
4. The generation of uranium series disequilibria by partial melting of spinel peridotite: constraints from partitioning studies;Beattie;Earth Planet. Sci. Lett.,1993
5. Experimental and natural partitioning of Th, U, Pb and other trace elements between garnet, clinopyroxene and basaltic melts;Hauri;Chem. Geol.,1994
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