Models of U-series disequilibria generation in MORB: the effects of two scales of melt porosity
- 1 October 2000
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 121 (3-4) , 189-204
- https://doi.org/10.1016/s0031-9201(00)00168-0
Abstract
No abstract availableKeywords
This publication has 43 references indexed in Scilit:
- Geophysical Constraints on Mantle Flow and Melt Generation Beneath Mid-Ocean RidgesPublished by Wiley ,2013
- Permeability of partially molten upper mantle rocks from experiments and percolation theoryJournal of Geophysical Research, 1997
- Constraints on mantle melting at mid-ocean ridges from global 238U–230Th disequilibrium dataNature, 1996
- Late-Stage Melt Evolution and Transport in the Shallow Mantle beneath the East Pacific RisePublished by International Ocean Discovery Program (IODP) ,1996
- Mixing of magmas from enriched and depleted mantle sources in the northeast Pacific: West Valley segment, Juan de Fuca RidgeContributions to Mineralogy and Petrology, 1995
- Uranium–thorium disequilibria and partitioning on melting of garnet peridotiteNature, 1993
- 231Pa and230Th chronology of mid-ocean ridge basaltsEarth and Planetary Science Letters, 1993
- Geochronology and petrogenesis of MORB from the Juan de Fuca and Gorda ridges by 238U– 230Th disequilibriumEarth and Planetary Science Letters, 1991
- U&z.sbnd;Th isotopic systematics at 13°N east Pacific Ridge segmentEarth and Planetary Science Letters, 1990
- Geochemical and structural studies of the Lamont seamounts: seamounts as indicators of mantle processesEarth and Planetary Science Letters, 1988