Comment on ‘Isotopic anomalies of noble gases in meteorites and their origins: 2. Separated minerals from Allende’ by Roy S. Lewis, Jacques Gros, and Edward Anders | Zendy

Manuel O. K. | Zendy

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Comment on ‘Isotopic anomalies of noble gases in meteorites and their origins: 2. Separated minerals from Allende’ by Roy S. Lewis, Jacques Gros, and Edward Anders

Author(s) -

Manuel O. K.

Publication year - 1979

Publication title -

journal of geophysical research: solid earth

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 1.67

H-Index - 298

eISSN - 2156-2202

pISSN - 0148-0227

DOI - 10.1029/jb084ib10p05683

Subject(s) - noble gas , allende meteorite , meteorite , xenon , component (thermodynamics) , chemistry , mineralogy , materials science , atomic physics , astrobiology , physics , chondrite , thermodynamics

Correlations between elemental and isotopic ratios of noble gases in mineral separates of Allende are not consistent with the reported identification of a noble gas component trapped in ‘Q’ with 136 Xe/ 132 Xe = 0.310 and 20 Ne/ 132 /Xe = 10 ± 4. If Q trapped a noble gas component with 136 Xe/ 132 Xe = 0.310, then the correlations indicate that there was no Ne in this gas component. If Q trapped a noble gas component with 20 Ne/ 132 Xe = 10 ± 4, then the correlations indicate that Q contains no fission Xe.

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