Time-dependent models of U–Th–He and K–Ar evolution and the layering of mantle convection
- 15 April 1998
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 145 (3-4) , 413-429
- https://doi.org/10.1016/s0009-2541(97)00152-6
Abstract
No abstract availableKeywords
This publication has 65 references indexed in Scilit:
- Rare gas systematics: formation of the atmosphere, evolution and structure of the Earth's mantlePublished by Elsevier ,2002
- Mineral-aqueous fluid partitioning of trace elements at 900°C and 2.0 GPa: Constraints on the trace element chemistry of mantle and deep crustal fluidsPublished by Elsevier ,2000
- The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust systemEarth and Planetary Science Letters, 1997
- The argon constraints on mantle structureGeophysical Research Letters, 1996
- Introduction to Geochemical ModelingPublished by Cambridge University Press (CUP) ,1995
- Short-Lived Chemical Heterogeneities in the Archean Mantle with Implications for Mantle ConvectionScience, 1994
- Solubility and partitioning of Ar in anorthite, diopside, forsterite, spinel, and synthetic basaltic liquidsGeochimica et Cosmochimica Acta, 1990
- Chemical composition of the mantleJournal of Geophysical Research, 1983
- Constraints on evolution of Earth's mantle from rare gas systematicsNature, 1983
- Isotopic evolution of the mantle: a modelEarth and Planetary Science Letters, 1982