TY - JOUR
T1 - Mafic silicate mapping on Mars
T2 - Effects of palagonitic material, multiple mafic silicates, and spectral resolution
AU - Cloutis, Edward A.
AU - Bell, James F.
N1 - Funding Information:
We thank Dr. Ted Roush at the NASA Ames Research Center and Dr. Dick Morris at the NASA Johnson Space Center, and the staff at the Smithsonian Institution National Museum of Natural History for providing the palagonitic materials and some of the mineral samples used in this study. We also thank Dr. Takahiro Hiroi and Dr. Carlé Pieters for providing generous access to the NASA-supported RELAB spectrometer facility for the spectral measurements. X-ray diffraction data were acquired and analyzed through the generous support and assistance of Dr. Frank Hawthorne and Mr. Neil Ball of the Department of Geological Sciences at the University of Manitoba. The authors also thank Mr. Trevor Mueller for his assistance with the spectral data analysis. This study was supported by a start-up and discretionary grant from the University of Winnipeg, and research grants from Sigma Xi and the Geological Society of America to EAC, and by a grant from the NASA Planetary Geology and Geophysics Program (NAG5-10636) to JFB. Sincere thanks to Janice Bishop and Scott Murchie for their thorough reviews and thoughtful comments on a sometimes dense manuscript and for pointing out some apparent shortcomings.
PY - 2004/11
Y1 - 2004/11
N2 - The visible to near-infrared spectral reflectance properties of intimate and areal pyroxene + palagonitic material mixtures as well as pure mafic silicates (low-calcium pyroxene, high-calcium pyroxene, pigeonite, olivine) and mixtures of these minerals were analyzed at high spectral resolution (5 nm) as well as with non-contiguous band passes equivalent to recent HST observations and the Pathfinder IMP in order to determine the quality and quantity of mineralogical information (end member compositions, abundances, and grain sizes) derivable in the presence of palagonitic material. In the case of pyroxene + palagonitic material mixtures, pyroxene is detectable at abundances as low as 10 wt%, and its composition can be constrained because (a) its diagnostic absorption feature (located near 1000 nm) persists even for high palagonitic material abundances, and (b) palagonitic material does not appreciably alter the wavelength position of this band (<4 nm variation). For broad band data (such as Pathfinder IMP band passes), different mafic silicates can be discriminated and palagonitic material abundances constrained using a variety of reflectance ratios and three-point "absorption band depths." However, other properties of mafic silicate ± palagonitic material assemblages, such as mafic silicate major element compositions, grain sizes, and end member abundances, generally cannot be rigorously quantified. The use of multiple reflectance ratios can, however, be used to identify relative changes in these properties, as most changes in mafic silicate ± palagonitic material assemblage properties are characterized by a unique corresponding set of reflectance ratio variations. The observed spectral-assemblage property trends are consistent with those expected from the known spectral properties of the end members.
AB - The visible to near-infrared spectral reflectance properties of intimate and areal pyroxene + palagonitic material mixtures as well as pure mafic silicates (low-calcium pyroxene, high-calcium pyroxene, pigeonite, olivine) and mixtures of these minerals were analyzed at high spectral resolution (5 nm) as well as with non-contiguous band passes equivalent to recent HST observations and the Pathfinder IMP in order to determine the quality and quantity of mineralogical information (end member compositions, abundances, and grain sizes) derivable in the presence of palagonitic material. In the case of pyroxene + palagonitic material mixtures, pyroxene is detectable at abundances as low as 10 wt%, and its composition can be constrained because (a) its diagnostic absorption feature (located near 1000 nm) persists even for high palagonitic material abundances, and (b) palagonitic material does not appreciably alter the wavelength position of this band (<4 nm variation). For broad band data (such as Pathfinder IMP band passes), different mafic silicates can be discriminated and palagonitic material abundances constrained using a variety of reflectance ratios and three-point "absorption band depths." However, other properties of mafic silicate ± palagonitic material assemblages, such as mafic silicate major element compositions, grain sizes, and end member abundances, generally cannot be rigorously quantified. The use of multiple reflectance ratios can, however, be used to identify relative changes in these properties, as most changes in mafic silicate ± palagonitic material assemblage properties are characterized by a unique corresponding set of reflectance ratio variations. The observed spectral-assemblage property trends are consistent with those expected from the known spectral properties of the end members.
KW - Mars surface
KW - Mineralogy
KW - Regoliths
KW - Spectrophotometry
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U2 - 10.1016/j.icarus.2004.06.002
DO - 10.1016/j.icarus.2004.06.002
M3 - Article
AN - SCOPUS:7444235873
SN - 0019-1035
VL - 172
SP - 233
EP - 254
JO - Icarus
JF - Icarus
IS - 1 SPEC.ISS.
ER -