Published for geochemistry community from Geochemical Society of Japan.
Xenology: The enigma of xenon in carbonaceous chondrites
Geochemical Journal, Vol. 10, No. 3, P. 121-136, 1976
ABSTRACT
The isotopic composition of the enigmatic xenon component (the so-called Renazzo-type fission xenon, CCF or X), which is said to be released from carbonaceous chondrites at temperatures 600 to 1, 000°C, is explained in terms of the variation of the isotopic ratios due to a combined effect of massfractionation, neutron capture and cosmic-ray irradiation processes, which took place during the early history of the solar system.- Published : 1976-09-20
- Released on J-STAGE : -
- Received : 1976/07/04
- Accepted : -
- DOI : https://doi.org/10.2343/geochemj.10.121
- J-STAGE URL : https://www.jstage.jst.go.jp/article/geochemj1966/10/3/10_3_121/_article/-char/ja
- J-Online ISSN: 1880-5973
- Print ISSN : 0016-7002
- ISSN-L : 0016-7002
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