Primitive Solar System materials and Earth share a common initial 142Nd abundance

A. Bouvier () and M. Boyet
Additional contact information
A. Bouvier: University of Western Ontario, Centre for Planetary Science and Exploration
M. Boyet: Clermont Université, Université Blaise Pascal, Laboratoire Magmas et Volcans, UMR CNRS 6524, Campus Universitaire des Cézeaux

Nature, 2016, vol. 537, issue 7620, 399-402

Abstract: Calcium–aluminium-rich refractory inclusions without isotopic anomalies in neodymium and enstatite chondrites share a 146Sm–142Nd isotopic evolution with the modern Earth’s mantle, supporting a chondritic Sm/Nd ratio for Earth.

Date: 2016
References: Add references at CitEc
Citations:

Downloads: (external link)
https://www.nature.com/articles/nature19351 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:7620:d:10.1038_nature19351

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

DOI: 10.1038/nature19351

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 ().