Incompatible trace elements in OIB and MORB and source enrichment in the sub-oceanic mantle-Reference-Cited by-同舟云学术

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Incompatible trace elements in OIB and MORB and source enrichment in the sub-oceanic mantle

Published:1995-07 Issue:3-4 Volume:133 Page:379-395
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Halliday Alex N.,Lee Der-Chuen,Tommasini Simone,Davies Gareth R.,Paslick Cassi R.,Godfrey Fitton J.,James Dodie E.

Publisher

Elsevier BV

Subject

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

Reference73 articles.

1. K, U and Th in mid-ocean ridge basalt glasses and heat production, KU and KRb in the mantle;Jochum;Nature,1983

2. Ba, Rb and Cs in the earth's mantle;Hofmann;Z. Naturforsch.,1983

3. Nb and Pb in oceanic basalts: New constraints on mantle evolution;Hofmann;Earth Planet. Sci. Lett.,1986

4. Siderophile and chalcophile element abundances in oceanic basalts, Pb isotope evolution and growth of the earth's core;Newsom;Earth Planet. Sci. Lett.,1986

5. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes;Sun,1989

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