Extreme geochemical fractionation during mantle melting: Insights from Hf-Nd isotopically ultra-depleted eclogite-Reference-Cited by-同舟云学术

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Extreme geochemical fractionation during mantle melting: Insights from Hf-Nd isotopically ultra-depleted eclogite

Published:2024-11 Issue:6 Volume:15 Page:101892
ISSN:1674-9871
Container-title:Geoscience Frontiers
language:en
Short-container-title:Geoscience Frontiers

Author:

Zhou Kun,Chen Yi-Xiang^ORCID,Zheng Yong-Fei,Chen Ren-Xu,Yang Yueheng

Funder

NSFC

Publisher

Elsevier BV

Reference74 articles.

1. Origins of xenolithic eclogites and pyroxenites from the Central Slave Craton, Canada.;Aulbach;J. Petrol.,2007

2. Microxenoliths from the Slave craton: Archives of diamond formation along fluid conduits;Aulbach;Lithos,2011

3. Trace-element mobilization during Ca-metasomatism along a major fluid conduit: Eclogitization of blueschist as a consequence of fluid–rock interaction;Beinlich;Geochim. Cosmochim. Acta,2010

4. Hf–Nd isotope decoupling in the oceanic lithosphere: constraints from spinel peridotites from Oahu, Hawaii;Bizimis;Earth Planet. Sci. Lett.,2004

5. A new digestion and chemical separation technique for rapid and highly reproducible determination of Lu/Hf and Hf isotope ratios in geological materials by MC-ICP-MS;Bizzarro;Geostand. Newslett.,2003

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