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Fission Xenon on MarsFission Xe components due to Pu-244 decay in the early history of Mars have been identified in nakhlites; as in the case of ALH84001 and Chassigny the fission gas was assimilated into indigenous solar-type Xe. Additional information is contained in the original extended abstract.
Document ID
20020045962
Acquisition Source
Goddard Space Flight Center
Document Type
Conference Paper
Authors
Mathew, K. J.
(California Univ., San Diego La Jolla, CA United States)
Marti, K.
(California Univ., San Diego La Jolla, CA United States)
Marty, B.
(Centre de Recherches Petrographiques et Geochimiques Nancy, France)
Date Acquired
August 20, 2013
Publication Date
April 1, 2002
Publication Information
Publication: Lunar and Planetary Science XXXIII
Subject Category
Lunar And Planetary Science And Exploration
Funding Number(s)
CONTRACT_GRANT: NAG5-8167
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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