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Possible Ni-Rich Mafic-Ultramafic Magmatic Sequence in the Columbia Hills: Evidence from the Spirit RoverThe Spirit rover landed on geologic units of Hesperian age in Gusev Crater. The Columbia Hills rise above the surrounding plains materials, but orbital images show that the Columbia Hills are older [1, 2]. Spirit has recently descended the southeast slope of the Columbia Hills doing detailed measurements of a series of outcrops. The mineralogical and compositional data on these rocks are consistent with an interpretation as a magmatic sequence becoming increasingly olivine-rich down slope. The outcrop sequence is Larry s Bench, Seminole, Algonquin and Comanche. The "teeth" on the Rock Abrasion Tool (RAT) wore away prior to arrival at Larry s Bench; the data discussed are for RAT brushed surfaces.
Document ID
20080026263
Acquisition Source
Johnson Space Center
Document Type
Conference Paper
Authors
Mittlefehldt, David W.
(NASA Johnson Space Center Houston, TX, United States)
Gellert, R.
(Guelph Univ. Ontario, Canada)
McCoy, T.
(Smithsonian Institution United States)
McSween, H. Y., Jr.
(Tennessee Univ. TN, United States)
Li, R.
(Ohio State Univ. United States)
Date Acquired
August 24, 2013
Publication Date
March 13, 2006
Subject Category
Geophysics
Meeting Information
Meeting: 37th Lunar and Planetary Science Conference
Location: League City, TX
Country: United States
Start Date: March 13, 2006
End Date: March 17, 2006
Distribution Limits
Public
Copyright
Public Use Permitted.
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