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Solid C triple bond N bearing material on outer solar system bodiesRecent telescopic observations have led to the identification of cyanogroup-containing molecules in the dark surface solids of several D-class asteroids, cometary dusts, and the rings of Uranus, as well as the low-albedo atmosphere of Iapetus. The occurrence of the 2.2-micron overtone of C triple-bond N's stretching fundamental mode in all four classes of small solar system bodies is presently suggested to serve as a diagnostic of both exposure duration and degree of modification of surface materials.
Document ID
19920035364
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Cruikshank, Dale P.
(NASA Ames Research Center Moffett Field, CA; NASA, Infrared Telescope Facility, Mauna Kea, HI, United States)
Allamandola, L. J.
(NASA Ames Research Center Moffett Field, CA, United States)
Hartmann, William K.
(NASA Infrared Telescope Facility, Mauna Kea, HI; Planetary Science Institute, Tucson AZ, United States)
Tholen, D. J.
(NASA Infrared Telescope Facility, Mauna Kea, HI; Hawaii, University Honolulu, United States)
Brown, R. H.
(JPL Pasadena, CA, United States)
Matthews, C. N.
(Illinois, University Chicago, United States)
Bell, J. F.
(Hawaii, University Honolulu, United States)
Date Acquired
August 15, 2013
Publication Date
December 1, 1991
Publication Information
Publication: Icarus
Volume: 94
ISSN: 0019-1035
Subject Category
Lunar And Planetary Exploration
Accession Number
92A17988
Distribution Limits
Public
Copyright
Other

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