Chondrites: Initial Strontium-87/Strontium-86 Ratios and the Early History of the Solar System

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Scientific paper

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.

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