Exposure Ages, Noble Gases and Nitrogen in the Ordinary Chondrite Karimati (L5)

Noble gas and nitrogen isotopic compositions of Karimati ordinary (L5) chondrite are presented. Aliquots of the meteorite were studied in two noble gas mass spectrometers. Its cosmic ray exposure (CRE) history, trapped noble gases and nitrogen isotopic systematic are examined. The compositions of Ne...

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Published inEarth, moon, and planets Vol. 124; no. 1-2; pp. 3 - 13
Main Author Mahajan, Ramakant R.
Format Journal Article
LanguageEnglish
Published Dordrecht Springer Netherlands 01.07.2020
Springer Nature B.V
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Summary:Noble gas and nitrogen isotopic compositions of Karimati ordinary (L5) chondrite are presented. Aliquots of the meteorite were studied in two noble gas mass spectrometers. Its cosmic ray exposure (CRE) history, trapped noble gases and nitrogen isotopic systematic are examined. The compositions of Ne and Kr in this meteorite indicate presence of mixture of solar wind and Q trapped components. In addition to the primordial components, radiogenic 129 Xe (from the decay of short-lived radioactive 129 I) is observed in the two aliquots ( 129 Xe/ 132 Xe ranges between 1.054 and 1.311). The U/Th- 4 He and K- 40 Ar ages are discordant. U/Th- 4 He ages are younger than the K- 40 Ar ages, indicating loss of helium. The trapped N component is isotopically light analogous to Q gas/solar wind. The cosmic-ray exposure ages of the two aliquots are 16.1 ± 2.7 Ma and 16.6 ± 2.0 Ma based on the cosmogenic 21 Ne c and 38 Ar c concentrations.
ISSN:0167-9295
1573-0794
DOI:10.1007/s11038-020-09532-w