Noble gases in SNC meteorites: Shergotty, Nakhla, Chassigny
- Max-Planck Institut fuer Chemie, Mainz (West Germany)
The author reports the elemental and isotopic composition of the noble gases in various fragments of the Shergotty, Nakhla, and Chassigny meteorites. Conclusions presented earlier which were based on results for trapped Ar, Kr and Xe only, are reaffirmed by the complete set of data. Arguments are presented that Chassigny-type gases are a better choice than (fractionated) terrestrial air for the second component, that, when mixed with SPB-gases produces the Shergotty composition. The ratios {sup 40}Ar/{sup 36}Ar{sub t} and {sup 40}Ar/{sup 129}Xe* in Shergotty agree with the respective values for EETA 79001 glass. This is taken as evidence for a late introduction of the supposedly shock implanted atmospheric component into Shergotty; it is at odds with scenarios that introduce the atmospheric component {approximately}180 m.y. ago. Based on the variable ratio {sup 40}Ar/{sup 129}Xe* and its unshocked nature, Nakhla acquired its excess {sup 129}Xe by a different process. {sup 21}Ne-based cosmic-ray exposure ages agree well with values in the literature, but do not readily agree with the younger ages based on the abundance of cosmogenic {sup 126}Xe. Neutron capture products are present in Nakhla Kr and there is evidence for a fission-like component in Xe of both Shergotty and Nakhla. GCR interactions with the SPB are unlikely to be the reason for the low {sup 36}Ar/{sup 38}Ar ratio in SPB-Ar.
- OSTI ID:
- 5222239
- Journal Information:
- Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 52:7; ISSN GCACA; ISSN 0016-7037
- Country of Publication:
- United States
- Language:
- English
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