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- W2139096994 abstract "We have measured the K41 and Ar40 contents of the metal phase of several iron meteorites, using activation analysis, and have obtained ages of 0–15 × 109 years. Shocked and unshocked specimens of Canyon Diablo show no differences in Ar content or K: Ar age. The K in the metal phase is located primarily along grain boundaries and is easily leached out by water. We conclude that ages previously measured by this technique are invalid in that they reflect mainly K loss by terrestrial water rather than an event in the meteorites formation." @default.
- W2139096994 created "2016-06-24" @default.
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- W2139096994 date "1968-08-15" @default.
- W2139096994 modified "2023-09-23" @default.
- W2139096994 title "Potassium: Argon problem in iron meteorites" @default.
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- W2139096994 doi "https://doi.org/10.1029/jb073i016p05429" @default.
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