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Inorganic analyses of Martian surface samples at the Viking landing sitesElemental analyses of fines in the Martian regolith at two widely separated landing sites, Chryse Planitia and Utopia Planitia, produced remarkably similar results. At both sites, the uppermost regolith contains abundant Si and Fe, with significant concentrations of Mg, Al, S, Ca, and Ti. The S concentration is one to two orders of magnitude higher, and K (less than 0.25% by weight) is at least 5 times lower than the average for earth's crust. The trace elements Sr, Y, and possibly Zr have been detected at concentrations near or below 100 parts per million. Pebble-sized fragments sampled at Chryse contain more S than the bulk fines and are thought to be pieces of a sulfate-cemented duricrust.
Document ID
19770033055
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Clark, B. C.
(Geological Survey Reston, VA, United States)
Castro, A. J.
(Geological Survey Reston, VA, United States)
Rowe, C. D.
(Martin Marietta Aerospace Denver, Colo., United States)
Baird, A. K.
(Geological Survey Reston, VA, United States)
Evans, P. H.
(Pomona College Claremont, Calif., United States)
Rose, H. J., Jr.
(Geological Survey Reston, VA, United States)
Toulmin, P., III
(U.S. Geological Survey Reston, Va., United States)
Keil, K.
(New Mexico, University Albuquerque, N. Mex., United States)
Kelliher, W. C.
(NASA Langley Research Center Hampton, Va., United States)
Date Acquired
August 9, 2013
Publication Date
December 17, 1976
Publication Information
Publication: Science
Volume: 194
Subject Category
Lunar And Planetary Exploration
Accession Number
77A15907
Funding Number(s)
CONTRACT_GRANT: NAS1-9000
CONTRACT_GRANT: NAS1-11858
CONTRACT_GRANT: NASA ORDER L-9717
CONTRACT_GRANT: NAS1-11855
Distribution Limits
Public
Copyright
Other

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