Interesting read from ASU - with supporting details and fascinating info 
regarding Allende's CAIs 

http://asunews.asu.edu/20091231_brennecka
 
 
http://www.sciencemag.org/cgi/content/abstract/science.1180871
 
 
Published Online December 31, 2009
Science DOI: 10.1126/science.1180871   
Reports
238U/235U Variations in Meteorites: Extant 247Cm and Implications for Pb-Pb 
DatingG. A. Brennecka,1, S. Weyer,2, M. Wadhwa,1 P. E. Janney,1 J. Zipfel,3 A. 
D. Anbar1,4 
The 238U/235U isotope ratio has long been considered invariantin meteoritic 
materials (i.e., 137.88). This assumption is acornerstone of the high-precision 
Pb-Pb dates that define theabsolute age of the Solar System. 
Calcium-aluminum-rich inclusionsof the Allende meteorite display variable 
238U/235U ratios,ranging between 137.409±0.039 and 137.885±0.009.This range 
implies substantial uncertainties in the ages previouslydetermined by Pb-Pb 
dating of CAIs, which may be overestimatedby several million years. The 
correlation of U isotope ratioswith proxies for Cm/U (i.e., Th/U and Nd/U) 
provides strongevidence that the observed variations of 238U/235U in CAIs 
wereproduced by the decay of extant 247Cm to 235U in the early SolarSystem, 
with an initial 247Cm/235U of ~ 1.1 to 2.4 x 10-4.
 1 School of Earth and Space Exploration, Arizona State University, Tempe, AZ 
85287, USA.
2 Institut fur Geowissenschaften, Goethe-Universität, Frankfurt, Germany.
3 Senckenberg Forschungsinstitut und Naturmuseum, Frankfurt, Germany.
4 Department of Chemistry and Biochemistry, Arizona State University, Tempe, AZ 
85287, USA. 
 Current address: Institut für Geology und Mineralogie,Universität zu Köln, 
Cologne, Germany.
 To whom correspondence should be addressed. E-mail: brenne...@asu.edu 
________________________________
Received for publication 20 August 2009. Accepted for publication 11 December 
2009.


      
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