Cosmogenic nuclides in the Kirin chondrite

Details Cosmogenic nuclides in the Kirin chondrite Cosmogenic nuclides in the Kirin chondrite

Jan 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982e%26psl..57..101h&link_type=abstract

Earth and Planetary Science Letters, vol. 57, no. 1, Jan. 1982, p. 101-109.

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Chondrites, Cobalt 60, Cosmochemistry, Manganese Isotopes, Meteoritic Composition, Sodium 22, Aluminum 26, Cosmic Rays, Cosmology, Irradiation, Japan, Potassium 40, Radiation Effects, Radioactivity, Rare Gases, Size (Dimensions), Meteorites, H5 Chondrites, Kirin Meteorite, Cosmogenic Elements, Nuclides, Ordinary Chondrites, Experiments, Data, Comparisons, Samples, Meteorite, Geometry, Manganese 53, Neon 21, Potassium 40, Isotopes

Scientific paper

Radioactive and stable cosmogenic nuclides have been determined in the various fragments of the Kirin chondrite (H5). Experimental results obtained from samples are described and compared with similar data obtained in other laboratories. Cosmogenic Mn-54, Na-22, Co-60, Al-26, Mn-53, K-40 (in the metal phase), and light noble gases were measured. Based on these data, the irradiation history of this meteorite can be explained in terms of a multi-stage exposure which involves a first-stage irradiation for 10 to the 7th years and a second stage for about 4 x 10 to the 5th years, and depth effects in the productions of the nuclides in 4 pi (second stage) and 2 (first stage) geometries.

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