Siderophile and chalcophile element abundances in oceanic basalts, Pb isotope evolution and growth of the Earth's core
- 23 October 2002
- journal article
- Published by Elsevier
- Vol. 80 (3-4) , 299-313
- https://doi.org/10.1016/0012-821x(86)90112-3
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- Hydrothermal uranium uptake at ridge crestsNature, 1985
- The depletion of siderophile elements in the Earth's mantle: new evidence from molybdenum and tungstenEarth and Planetary Science Letters, 1984
- K, U and Th in mid-ocean ridge basalt glasses and heat production, K/U and K/Rb in the mantleNature, 1983
- Hafnium isotope results from mid-ocean ridges and KerguelenLithos, 1983
- Chemical aspects of the formation of the corePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1982
- Sr and Nd isotope geochemistry of oceanic basalts and mantle evolutionNature, 1982
- Terrestrial lead isotopic evolution and formation time of the Earth's coreNature, 1977
- Lead isotope measurements from the oldest recognised Lewisian gneisses of north-west ScotlandNature, 1977
- Nd isotopic variations and petrogenetic modelsGeophysical Research Letters, 1976
- Comportement Des Systemes U-Th-Pb Dans Le Manteau Superieur Et Modele d'Evolution De Ce Dernier Au Cours Des Temps GeologiquesEarth and Planetary Science Letters, 1968