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      The case for a martian origin of the shergottites: nitrogen and noble gases in EETA 79001

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      Earth and Planetary Science Letters
      Elsevier BV

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          The composition of the atmosphere at the surface of Mars

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            Composition and structure of Mars' Upper atmosphere: Results from the neutral mass spectrometers on Viking 1 and 2

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              Martian Gases in an Antarctic Meteorite?

              Significant abundances of trapped argon, krypton, and xenon have been measured in shock-altered phases of the achondritic meteorite Elephant Moraine 79001 from Antarctica. The relative elemental abundances, the high ratios of argon-40 to argon-36 (>/= 2000), and the high ratios of xenon-129 to xenon-132 (>/= 2.0) of the trapped gas more closely resemble Viking data for the martian atmosphere than data for noble gas components typically found in meteorites. These findings support earlier suggestions, made on the basis of geochemical evidence, that shergottites and related rare meteorites may have originated from the planet Mars.
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                Author and article information

                Journal
                Earth and Planetary Science Letters
                Earth and Planetary Science Letters
                Elsevier BV
                0012821X
                August 1984
                August 1984
                : 69
                : 2
                : 225-242
                Article
                10.1016/0012-821X(84)90183-3
                557ae72f-3182-4883-aa40-f64e902097c1
                © 1984

                http://www.elsevier.com/tdm/userlicense/1.0/

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