Spectroscopic observation of Mars

Advances in Space Research

Volumn 5, Issue 8, 1985, Pages 59-68

  Singer, Robert B ^a  

^a UNIVERSITY OF HAWAII   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0002380282     PISSN: 02731177     EISSN: None     Source Type: Journal    
DOI: 10.1016/0273-1177(85)90242-X     Document Type: Article

References (46)

1. Mars surface composition from reflectance spectroscopy: A summary
2. Mars Narrowband Photometry from 03 to 25 microns of surface regions during the 1969 apparition
3. Mars Near-infrared reflectance spectra of surface regions and compositional implication
4. First direct detection of clay minerals on Mars
5. Spectral Reflectance of Martian areas during the 1973 opposition: Photoelectric filter photometry 0.33–1.10μm
6. Color changes at the Viking landing sites over the course of a Mars year
7. The dark materials on Mars: 1. New information from reflectance spectroscopy on the extent and mode of oxidation
8. Spectral evidence for the minerology of high-albedo soils and dust on Mars
9. Spectral characteristics of the iron oxides with application to the Martian bright region mineralogy
10. 2O liquid-ice interfaces in the martian crust
11. Geochemical and mineralogical interpretation of the Viking inorganic chemical results
12. Alteration of glass as a possible source of clay minerals on Mars
13. Amorphous gels as possible analogs to Martian weathering products
14. Comparison of Viking Lander multispectral images and laboratory reflectance spectra of terrestrial samples
15. Altered basaltic glass: A terrestrial analog to the soil of Mars
16. 5+ mineralogy of Mars
17. Global color variations on the martian surface
18. Mars Definition and characterization of global surface units with emphasis on composition
19. On the composition of martian surface material
20. Astronomical infrared spectroscopy with a Connes-type interferometer: II. Mars, 2500–3500 cm-1
21. Evidence about hydrate and solid water in the martian surface from the 1969 Mariner infrared spectrometer
22. Investigation of the martian environment by infrared spectroscopy on Mariner 9
23. Mars: Components of infrared spectra and composition of the dust cloud
24. Composition of the martian dust as derived by infrared spectroscopy from Mariner 9
25. Physical properties of the particles composing the martian dust storm of 1971–1972
26. Visible and near-infrared spectra of minerals and rocks, I, Silicate minerals
27. Spectral signatures of particulate minerals in the visible and nearinfrared
28. Remote sensing for exploration: An overview
29. Spectral reflectance of carbonate minerals and rocks in the visible and near-infrared (0.35–2.55μm): Applications in carbonate petrology
30. Mars Interpretation of spectral reflectivity of light and dark regions
31. Mars: Large scale mixing of bright and dark surface materials and implications for analysis of spectral reflectance
32. Diffuse reflectance spectra of pigmentary-sized iron oxides, iron oxyhydroxides, and their mixtures: implications for the reflectance spectra of Mars
33. Effects of iron silica gels on spectral reflectance
34. Spectral reflectance properties of particulate weathered coatings on rocks: Laboratory modeling and applicability to Mars
35. The mantle of Mars: Some possible geologic implications of its high density
36. Interpretation of visible and near-infrared diffuse reflectance spectra of pyroxenes and other rock-forming minerals
37. Near-infrared spectra: reflectance of mineral mixtures Systematic combinations of pyroxenes, olivine, and iron oxides
38. Mars: Petrologic units in the Margaritifer Sinus and Coprates Quadrangle
39. The dark materials on Mars: II. New mineralogic interpretations from reflectance spectroscopy and petrologic implications
40. Multispectral analysis of the Kasei Vallis - Lunae Planum region of Mars
41. Water frost and ice: The near-infrared spectral reflectance 0.65–2.5μm
42. The spectral reflectance of water-mineral mixtures at low temperatures
43. Mars residual north polar cap Earth-based spectroscopic confirmation of water ice as a major constituent and evidence for hydrated minerals