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Problem of nature of inert gases in lunar surface materialThe origin of isotopes of inert gases in lunar surface material was investigated from the standpoint of the isotopic two-component status of inert gases in the solar system. Helium and neon represent the solar wind component, while krypton and xenon are planetary gases. Type A gases are trapped by the material of the regolith in the early stages of the existence of the solar system and were brought to the lunar surface together with dust. The material of the regolith therefore cannot be considered as the product of the erosion of the crystalline rocks of the moon and in this sense are extralunar. The regolith material containing type A gases must be identified with the high temperature minerals of the carbonaceous chondrites.
Document ID
19750003778
Acquisition Source
Legacy CDMS
Document Type
Other
Authors
Levskiy, L. K.
(Kanner (Leo) Associates Redwood City, CA, United States)
Date Acquired
August 8, 2013
Publication Date
October 1, 1974
Publication Information
Publication: Lunar soil from the Sea of Fertility (NASA-TT-F-15881)
Subject Category
Lunar And Planetary Exploration
Accession Number
75N11850
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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