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Shock-implanted noble gases. II - Additional experimental studies and recognition in naturally shocked terrestrial materialsThe process by which ambient gases can be implanted into silicates by shocks was investigated by analyzing the noble-gas content of several experimentally and naturally shocked silicate samples. The retentivity of shock-implanted gas during stepwise heating in the laboratory was defined in terms of two parameters, namely, the activation energy for diffusion and the extraction temperature at which 50 percent of the gas is released, both of which correlate with the shock pressure. The experiments indicate that, with increasing shock pressure, gas implantation occurs through an increasing production of microcracks/defects in the silicate lattice. The degree of annealing of these defects control the degree of diffusive loss of implanted gas.
Document ID
19890062575
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Bogard, Donald
(NASA Lyndon B. Johnson Space Center Houston, TX, United States)
Horz, Friedrich
(NASA Lyndon B. Johnson Space Center Houston, TX, United States)
Johnson, Pratt
(NASA Johnson Space Center Houston, TX, United States)
Date Acquired
August 14, 2013
Publication Date
June 1, 1989
Publication Information
Publication: Meteoritics
Volume: 24
ISSN: 0026-1114
Subject Category
Lunar And Planetary Exploration
Accession Number
89A49946
Distribution Limits
Public
Copyright
Other

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