Evidence of phyllosilicates in Wooly Patch, an altered rock encountered at West Spur, Columbia Hills, by the Spirit rover in Gusev crater, Mars
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Abstract
On its traverse to Columbia Hills, the Mars Exploration Rover Spirit investigated an outcrop designated “Wooly Patch” that exhibited morphological, mineralogical, and geochemical characteristics at the extreme ends of ranges observed among rocks studied at West Spur, a westward projecting salient near the foot of the Columbia Hills, Gusev crater. The major‐element composition and Fe‐mineralogy, as determined by the Alpha‐Particle X‐ray Spectrometer and Mössbauer Spectrometer, are inconsistent with any reasonable assemblage of basaltic minerals in that there is an excess of Si and Al. The combined data are best explained by the presence of 14–17% phyllosilicate minerals. Phyllosilicates that account for the composition and cation ratios include members of the kaolinite, serpentine, chlorite, and septechlorite groups. The potential existence of kaolinite‐type Al‐rich phyllosilicates within the Wooly Patch outcrop suggests a mildly acidic environment (pH 4–6) in the past and an open hydrologic system with good drainage conditions in the environment where these rocks were altered.
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Evidence of phyllosilicates in Wooly Patch, an altered rock encountered at West Spur, Columbia Hills, by the Spirit rover in Gusev crater, Mars |
Series title | Journal of Geophysical Research E: Planets |
DOI | 10.1029/2005JE002516 |
Volume | 111 |
Issue | E2 |
Year Published | 2006 |
Language | English |
Publisher | American Geophysical Union |
Publisher location | Washington, D.C. |
Contributing office(s) | Astrogeology Science Center |
Description | 22 p. |
Larger Work Type | Article |
Larger Work Subtype | Journal Article |
Larger Work Title | Journal of Geophysical Research E: Planets |
Other Geospatial | Columbia Hills; Gusev Crater; Mars; West Spur; Wooly Patch |
Google Analytic Metrics | Metrics page |