Uranium–thorium disequilibria and partitioning on melting of garnet peridotite
- 1 May 1993
- journal article
- Published by Springer Nature in Nature
- Vol. 363 (6424) , 63-65
- https://doi.org/10.1038/363063a0
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- 230Th238U disequilibrium and the melting processes beneath ridge axesPublished by Elsevier ,2002
- On the occurrence of apparent non-Henry's Law behaviour in experimental partitioning studiesGeochimica et Cosmochimica Acta, 1993
- Oceanic crustal thickness from seismic measurements and rare earth element inversionsJournal of Geophysical Research, 1992
- High-resolution garnet chronometry and the rates of metamorphic processesEarth and Planetary Science Letters, 1991
- Partial Melt Distributions from Inversion of Rare Earth Element ConcentrationsJournal of Petrology, 1991
- Melting in the oceanic upper mantle: An ion microprobe study of diopsides in abyssal peridotitesJournal of Geophysical Research, 1990
- The hafnium paradox and the role of garnet in the source of mid-ocean-ridge basaltsNature, 1989
- Effects of partial melting on the uranium decay seriesGeochimica et Cosmochimica Acta, 1989
- Melting of a dry peridotite KLB‐1 up to 14 GPa: Implications on the Origin of peridotitic upper mantleJournal of Geophysical Research, 1986
- Geochemical characteristics of mid-ocean ridge basaltsEarth and Planetary Science Letters, 1979