Space Science Reviews · 2012 · 275 citations · 31 references
Natural SciencesEarth SciencesGeologyElemental AnalysisGeochemistryPlanetary GeologyMartian GeologyMineral AnalysisMineral ChemistryMineral GeochemistryMineral IdentificationPlanetary MineralogyAlterationMars GeochemistryMars Rover InstrumentationMartian MineralogyMineral Alteration PathwaysMineral Content QuantificationMineralogical CharacterizationX-ray Fluorescence Spectroscopy
A principal goal of the Mars Science Laboratory (MSL) rover Curiosity is to identify and characterize past habitable environments on Mars. Determination of the mineralogical and chemical composition of Martian rocks and soils constrains their formation and alteration pathways, providing information on climate and habitability through time. The CheMin X-ray diffraction (XRD) and X-ray fluorescence (XRF) instrument on MSL will return accurate mineralogical identifications and quantitative phase abundances for scooped soil samples and drilled rock powders collected at Gale Crater during Curiosity's 1-Marsyear nominal mission. The instrument has a Co X-ray source and a cooled charge-coupled device (CCD) detector arranged in transmission geometry with the sample. CheMin's angular range of 5 to 50 2 with < 0.35 2 resolution is sufficient to identify and quantify virtually all minerals. CheMin's XRF requirement was descoped for technical and budgetary reasons. However, X-ray energy discrimination is still required to separate Co K from Co K and Fe K photons. The X-ray energy-dispersive histograms (EDH) returned along with XRD for instrument evaluation should be useful in identifying elements Z > 13 that are contained in the sample. The CheMin XRD is equipped with internal chemical and mineralogical standards and 27 reusable sample cells with either Mylar or Kapton windows to accommodate acidic-to-basic environmental conditions. The CheMin flight model (FM) instrument will be calibrated utilizing analyses of common samples against a demonstrationmodel (DM) instrument and CheMin-like laboratory instruments. The samples include phyllosilicate and sulfate minerals that are expected at Gale crater on the basis of remote sensing observations.
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Mars Surface Diversity as Revealed by the OMEGA/Mars Express Observations
Jean‐Pierre Bibring, Yves Langevin, A. Gendrin et al. · Science · 2005 · 956 citations
Phyllosilicates on Mars and implications for early martian climate
F. Poulet, J. P. Bibring, John F. Mustard et al. · Nature · 2005 · 947 citations
Natural Sciences, Astronomy, Geology +12
American mineralogist crystal structure database
Choice Reviews Online · 2004 · 897 citations
Sedimentary Rocks of Early Mars
M. C. Malin, K. S. Edgett · Science · 2000 · 841 citations