Siderophile and chalcophile element abundances in oceanic basalts, Pb isotope evolution and growth of the Earth's core-Reference-Cited by-同舟云学术

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Siderophile and chalcophile element abundances in oceanic basalts, Pb isotope evolution and growth of the Earth's core

Published:1986-11 Issue:3-4 Volume:80 Page:299-313
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Newsom H.E.,White W.M.,Jochum K.P.,Hofmann A.W.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference56 articles.

1. Sr and Nd isotope geochemistry of oceanic basalts and mantle evolution;White;Nature,1982

2. Nd isotopic variations and petrogenetic models;DePaolo;Geophys. Res. Lett.,1976

3. Hafnium isotope results from mid-ocean ridges and Kerguelen;Patchett;Lithos,1983

4. Approximation of terrestrial lead isotope evolution by a two-stage model;Stacey;Earth Planet. Sci. Lett.,1975

5. Terrestrial lead isotopic evolution and formation time of the Earth's core;Vollmer;Nature,1977

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