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Published August 1, 1988 | Version public
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Endemic silver isotopic anomalies in iron meteorites

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Abstract

The discovery of excess ^(107)Ag (^(107)Ag*) was made in a IVB iron meteorite ten years ago. The ^(107)Ag* anomaly is inferred to be due to decay of ^(107)pd (t_(1/2)=6.5 10^6 y) and appears to provide a chronometer for the timescale of early planet formation and differentiation.

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© 1988 Elsevier B.V.

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Eprint ID
42093
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CaltechAUTHORS:20131028-103005393

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Created
2013-10-28
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Updated
2021-11-10
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