EconPapers    
Economics at your fingertips  
 

Does U–Pb date Earth's core formation?; How well can Pb isotopes date core formation? (Reply)

B. J. Wood and A. N. Halliday ()
Additional contact information
B. J. Wood: Macquarie University
A. N. Halliday: University of Oxford

Nature, 2006, vol. 444, issue 7115, E2-E3

Abstract: Abstract Yin and Jacobsen 1 and Kamber and Kramers 2 highlight several issues to do with the tungsten (W) and lead (Pb) isotopic chronometry of terrestrial accretion and core segregation, although none of these affect our model or conclusions3. Yin and Jacobsen1 suggest that it is not clear from our analysis3 that 182Hf−182W provides a reliable system of chronometry for the bulk of core formation, whereas 235/238U−207/206Pb relates to the very last stage of sulphide segregation —which was exactly our point3 and is clarified here.

Date: 2006
References: Add references at CitEc
Citations:

Downloads: (external link)
https://www.nature.com/articles/nature05360 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:444:y:2006:i:7115:d:10.1038_nature05360

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

DOI: 10.1038/nature05360

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 ().

 
Page updated 2025-03-19
Handle: RePEc:nat:nature:v:444:y:2006:i:7115:d:10.1038_nature05360