Chondrites: Initial Strontium-87/Strontium-86 Ratios and the Early History of the Solar System
G. W. Wetherill 1,
R. Mark 1, and
C. Lee-Hu 1
1 Department of Planetary and Space Science, University of California, Los Angeles 90024
A sodium-poor, calcium-rich inclusion in the carbonaceous chondrite Allende had a 87Sr/86Sr ratio at the time of its formation of 0.69880, as low a value as that found in any other meteorite. The higher 87Sr/86Sr ratios found in ordinary chondrites indicate that their formation or isotopic equilibration occurred tens of millions of years later.