Spallogenic 14C in high-altitude rocks and in Antarctic meteorites

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Abstract

14C in high-altitude rocks and in Antarctic meteorites of long terrestrial age has been found at levels consistent with in-situ production by cosmic rays. Levels of 0.2-0.59 dpm/kg (or 1.0-2.6 × 10614C/g) are found in high-altitude samples ranging from 3300 to 5460 m. Similar values are observed in Antarctic meteorites that have been dated by 81Kr by Freundel, Schultz & Reedy (1986) as over 100 kyr old. -Authors

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Jull, A. J. T., Donahue, D. J., Linick, T. W., & Wilson, G. C. (1990). Spallogenic 14C in high-altitude rocks and in Antarctic meteorites. Radiocarbon, 31(3), 719–724. https://doi.org/10.1017/s0033822200012315

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