Reply [to “The mean life of continents is currently not constrained by Nd and Hf isotopes”]
- 1 February 1984
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 11 (2) , 154-155
- https://doi.org/10.1029/gl011i002p00154
Abstract
No abstract availableThis publication has 9 references indexed in Scilit:
- The mean life of continents is currently not constrained by Nd and Hf isotopesGeophysical Research Letters, 1984
- The mean life of continents: Estimates of continent recycling rates from Nd and Hf isotopic data and implications for mantle structureGeophysical Research Letters, 1983
- Sr and Nd isotope geochemistry of oceanic basalts and mantle evolutionNature, 1982
- Evolution of continental crust and mantle heterogeneity: Evidence from Hf isotopesContributions to Mineralogy and Petrology, 1982
- Columbia River volcanism: the question of mantle heterogeneity or crustal contaminationGeochimica et Cosmochimica Acta, 1981
- Nd and Sr isotopic study of the Bay of Islands Ophiolite Complex and the evolution of the source of midocean ridge basaltsJournal of Geophysical Research, 1979
- The mean age of mantle and crustal reservoirsJournal of Geophysical Research, 1979
- Basalt magma sources during the opening of the North AtlanticNature, 1979
- Neodymium isotopes in flood basalts from the Siberian Platform and inferences about their mantle sourcesProceedings of the National Academy of Sciences, 1979