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Jarosite and Hematite at Meridiani Planum from Opportunity's Mössbauer Spectrometer.
- Source :
-
Science . 12/3/2004, Vol. 306 Issue 5702, p1740-1745. 6p. 3 Charts, 7 Graphs. - Publication Year :
- 2004
-
Abstract
- Mössbauer spectrometers provide quantitative information about the distribution of iron among its oxidation states, the identification of iron-bearing phases, and the distribution of iron among those phases. Characterizing the speciation and distribution of iron in martian rock and soil [1] constrains primary rock types; the conditions under which primary minerals crystallize; and the mineralogical composition, process, and extent of alteration and weathering. Hematite (α-Fe[sub 2]O[sub 3]) was detected in Meridiani Planum from orbital observations before the Mars Exploration Rover (MER) missions [2, 3], and the region was selected as a MER landing site on a scientific basis, because the mineral is a beacon for aqueous processes, and on an engineering basis, because the terrain was considered safe for landing [4]. The first Mössbauer spectrum from Meridiani Planum was obtained by the Opportunity rover on 4 February 2004, on soil near the lander at Eagle crater. [ABSTRACT FROM AUTHOR]
- Subjects :
- *SPECTROMETERS
*IRON
*OXIDATION
*ROCKS
*SOILS
*MARS (Planet)
Subjects
Details
- Language :
- English
- ISSN :
- 00368075
- Volume :
- 306
- Issue :
- 5702
- Database :
- Academic Search Index
- Journal :
- Science
- Publication Type :
- Academic Journal
- Accession number :
- 15331289