The core of planet formation
Bill Minarik ()
Additional contact information
Bill Minarik: University of Maryland
Nature, 2003, vol. 422, issue 6928, 126-127
Abstract:
The rocky bodies from which the Earth formed may have already separated into a metal core and silicate shell. Innovative experiments exploring the behaviour of molten metal trapped between silicate grains suggest how.
Date: 2003
References: Add references at CitEc
Citations:
Downloads: (external link)
https://www.nature.com/articles/422126a 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:422:y:2003:i:6928:d:10.1038_422126a
Ordering information: This journal article can be ordered from
https://www.nature.com/
DOI: 10.1038/422126a
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 ().