The evolution of terrestrial volatiles: a view from helium, neon, argon and nitrogen isotope modelling
- 1 May 1998
- journal article
- conference paper
- Published by Elsevier in Chemical Geology
- Vol. 147 (1-2) , 27-52
- https://doi.org/10.1016/s0009-2541(97)00170-8
Abstract
No abstract availableKeywords
This publication has 104 references indexed in Scilit:
- Helium Isotopic Evidence for a Lower Mantle Component in Depleted Archean KomatiiteScience, 1996
- Limits on the mass flux between lower and upper mantle and stability of layeringEarth and Planetary Science Letters, 1996
- The 40Ar/36Ar ratio of the undepleted mantle; A reevaluationGeophysical Research Letters, 1995
- Constraints on rare gas partition coefficients from analysis of olivine-glass from a picritic mid-ocean ridge basaltChemical Geology, 1993
- Off-disk penetration of ancient solar windIcarus, 1991
- Evolution of a steam atmosphere during earth's accretionIcarus, 1988
- Noble-gas state in the earth's interior — Some constraints on the present stateChemical Geology: Isotope Geoscience section, 1985
- SrNd and ArHe isotopic relationships: Comparison, geotectonic implications and approximation by model computingChemical Geology: Isotope Geoscience section, 1985
- K, U and Th in mid-ocean ridge basalt glasses and heat production, K/U and K/Rb in the mantleNature, 1983
- Helium isotopic variations in the mantle beneath the central North Atlantic OceanEarth and Planetary Science Letters, 1982