The mean life of continents is currently not constrained by Nd and Hf isotopes
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v011/i002/GL011i002p00151/GL011i002p00151.pdf
Reference12 articles.
1. Radiogenic isotopes: the case for crustal recycling on a near-steady-state no-continental-growth Earth;Armstrong;Phil. Trans. R. Soc. Lond.,1981
2. Crustal growth and mantle evolution: inferences from models of element transport and Nd and Sr isotopes;DePaolo;Geochim. Cosmochim. Acta.,1980
3. The mean life of continents: estimates of continent recycling rates from Nd and Hf isotopic data and implications for mantle structure;DePaolo;Geophys. Res. Lett.,1983
4. Nd isotopic variations and petrogenetic models;DePaolo;Geophys. Res. Lett.,1976
5. An estimate of the Nd isotopic composition of Iapetus seawater from ca. 490 Ma metalliferous sediments;Hooker;Earth Planet. Sci. Lett.,1981
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