Final chemical results from the Mars Pathfinder alpha proton X-ray spectrometer

被引:97
作者
Foley, CN
Economou, T
Clayton, RN
机构
[1] Univ Chicago, Enrico Fermi Inst, Chicago, IL 60637 USA
[2] Univ Chicago, Lab Astrophys & Space Res, Chicago, IL 60637 USA
[3] Univ Chicago, Dept Geophys Sci, Chicago, IL 60637 USA
[4] Univ Chicago, Dept Chem, Chicago, IL 60637 USA
关键词
Mars Pathfinder; final chemical results; Martian rock and soil chemistry; alpha proton X-ray spectrometer; geochemistry;
D O I
10.1029/2002JE002019
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The calibrated Pathfinder alpha proton X-ray spectrometer (APXS) instrument is capable of measuring concentrations of all major and minor rock-forming elements ranging from carbon through zirconium in atomic number. Therefore it is capable of constraining the petrology of the measured samples. In particular, the Pathfinder data are the first in situ measurements of Martian rocks and may be compared with previous remote-sensing measurements as well as with the compositions of SNC meteorites. Pathfinder soil and rock sample abundances from the alpha, proton, and X-ray modes have been quantified. The abundances suggest that (1) the rocks are covered with various amounts of soil; (2) the soil-free rocks, on a volatile-free basis, have some element ratios similar to Mars meteorites, yet have different bulk chemistry indicative of more evolved rocks with higher silica abundances; (3) the carbon and nitrogen contents are below detection limits; and (4) the alpha mode oxygen reveals excess amounts of oxygen in some samples, which is indicative of sample-bound water (contained within minerals or glasses in samples).
引用
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页数:21
相关论文
共 61 条
[1]  
[Anonymous], 1990, PRINCIPLES IGNEOUS M
[2]   A global view of Martian surface compositions from MGS-TES [J].
Bandfield, JL ;
Hamilton, VE ;
Christensen, PR .
SCIENCE, 2000, 287 (5458) :1626-1630
[3]  
Banin A., 1992, Mars, P594
[4]  
Basaltic Volcanism Study Project, 1981, BAS VOLC TERR PLAN
[5]   THERMALLY ALTERED PALAGONITIC TEPHRA - A SPECTRAL AND PROCESS ANALOG TO THE SOIL AND DUST OF MARS [J].
BELL, JF ;
MORRIS, RV ;
ADAMS, JB .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 1993, 98 (E2) :3373-3385
[6]   Mineralogic and compositional properties of Martian soil and dust:: Results from Mars Pathfinder [J].
Bell, JF ;
McSween, HY ;
Crisp, JA ;
Morris, RV ;
Murchie, SL ;
Bridges, NT ;
Johnson, JR ;
Britt, DT ;
Golombek, MP ;
Moore, HJ ;
Ghosh, A ;
Bishop, JL ;
Anderson, RC ;
Brückner, J ;
Economou, T ;
Greenwood, JP ;
Gunnlaugsson, HP ;
Hargraves, RM ;
Hviid, S ;
Knudsen, JM ;
Madsen, MB ;
Reid, R ;
Rieder, R ;
Soderblom, L .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 2000, 105 (E1) :1721-1755
[7]   Ventifacts at the Pathfinder landing site [J].
Bridges, NT ;
Greeley, R ;
Haldemann, AFC ;
Herkenhoff, KE ;
Kraft, M ;
Parker, TJ ;
Ward, AW .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 1999, 104 (E4) :8595-8615
[8]   Characteristics of the Pathfinder APXS sites: Implications for the composition of Martian rocks and soils [J].
Bridges, NT ;
Crisp, JA ;
Bell, JF .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 2001, 106 (E7) :14621-14665
[9]  
BRIDGES NT, 2000, LUNAR PLANET SCI, V31
[10]   RATES AND MECHANISMS OF CHEMICAL-WEATHERING OF FERROMAGNESIAN SILICATE MINERALS ON MARS [J].
BURNS, RG .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1993, 57 (19) :4555-4574