The lead isotopic age of the Earth can be explained by core formation alone

Nature

Volumn 465, Issue 7299, 2010, Pages 767-770

  Wood, Bernard J ^a,b   Halliday, Alex N ^a  

^a UNIVERSITY OF OXFORD   (United Kingdom)

^b MACQUARIE UNIVERSITY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

CARBON; IRON; ISOTOPE; LEAD; SILICATE; VOLATILE AGENT;

ACCRETION; AGE DETERMINATION; ALLOY; CARBON; CORE (PLANETARY); IMPACT; IRON; ISOTOPIC ANALYSIS; LEAD ISOTOPE; MOON; SOLAR SYSTEM; VOLATILE ELEMENT;

ARTICLE; FRACTIONATION; PRIORITY JOURNAL; TEMPERATURE SENSITIVITY; THERMODYNAMICS;

EID: 77953474324     PISSN: 00280836     EISSN: 14764687     Source Type: Journal    
DOI: 10.1038/nature09072     Document Type: Article

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