Key new pieces of the HIMU puzzle from olivines and diamond inclusions

Yaakov Weiss (), Cornelia Class (), Steven L. Goldstein () and Takeshi Hanyu ()
Additional contact information
Yaakov Weiss: Lamont-Doherty Earth Observatory of Columbia University
Cornelia Class: Lamont-Doherty Earth Observatory of Columbia University
Steven L. Goldstein: Lamont-Doherty Earth Observatory of Columbia University
Takeshi Hanyu: Japan Agency for Marine-Earth Science and Technology

Nature, 2016, vol. 537, issue 7622, 666-670

Abstract: Trace-element analyses of olivine phenocrysts and diamond inclusions indicate that carbonatite-metasomatized subcontinental mantle may be the source of the HIMU mantle end-member, as opposed to recycled basaltic oceanic crust.

Date: 2016
References: Add references at CitEc
Citations: View citations in EconPapers (2)

Downloads: (external link)
https://www.nature.com/articles/nature19113 Abstract (text/html)
Access to the full text of the articles in this series is restricted.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:537:y:2016:i:7622:d:10.1038_nature19113

Ordering information: This journal article can be ordered from
https://www.nature.com/

DOI: 10.1038/nature19113

Access Statistics for this article

Nature is currently edited by Magdalena Skipper

More articles in Nature from Nature
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().