In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle-Reference-Cited by-同舟云学术

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In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle

Published:2005-08 Issue:7053 Volume:436 Page:1005-1008
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

Alard Olivier,Luguet Ambre,Pearson Norman J.,Griffin William L.,Lorand Jean-Pierre,Gannoun Abdelmouhcine,Burton Kevin W.,O'Reilly Suzanne Y.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/nature03902.pdf

Reference31 articles.

1. Hofmann, A. W. in The Mantle (ed. Carlson, R. W.) 61–101 (Elsevier, Oxford, 2004)

2. Snow, J., Hart, S. R. & Dick, H. B. J. Nd and Sr isotopic evidence for a link between mid-ocean ridge basalts and abyssal peridotites. Nature 371, 57–60 (1994)

3. Schiano, P., Birck, J.-L. & Allègre, C. J. Osmium-strontium-neodymium-lead isotopic covariations in mid-ocean ridge basalt glasses and the heterogeneity of the upper mantle. Earth Planet. Sci. Lett. 150, 363–379 (1997)

4. Roy-Barman, M. & Allègre, C. J. 187Os/186Os ratios of mid-ocean ridge basalts and abyssal peridotites. Geochim. Cosmochim. Acta 58, 5043–5054 (1994)

5. Snow, J. E. & Reisberg, L. Os isotope systematics of the MORB mantle: results from altered abyssal peridotites. Earth Planet. Sci. Lett. 133, 411–421 (1995)

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