The reflectance spectra of powdered samples of selected minerals, meteorites, lunar materials and frosts are presented as an aid in the interpretation of present and future remote sensing data of solar system objects. Spectra obtained in separate wavelength regions have been combined and normalized, yielding coverage from 92 to 1800 nm. Spectral features include reflectance maxima in the far UV region produced by valence-conduction interband transitions, and reflectance minima in the near UV, visible and near IR regions, produced by charge transfer and crystal field transitions. Specific maxima and minima are diagnostic of mineral type and composition; additionally, the minerals present in mixtures such as meteorites and lunar samples can b...
Diffuse reflectance spectra, 400-800 nm, were determined on minerals, goethite, hematite, ilmenite, ...
Supplemetary materials for the "Mapping the spectral and mineralogical variability of lunar breccia ...
Remote-sensing infrared spectroscopy is the principal field of investigation for planetary surfaces ...
A positive identification of the minerals olivine, plagioclase, and several types of pyroxenes were ...
We report the spectral reflectance of Martian meteorites from 0.3-2.6 microns for the purpose of cat...
Presented here are infrared reflectance spectra of a typical set of Apollo samples to illustrate spe...
The major mineralogical components of Yamato-791197 determined from reflectance spectra are calcium-...
For the last decade telescopic near infrared spectra have been obtained for small lunar areas. Such ...
Summary This dataset contains spectral reflectance values for laboratory mixtures that were created...
Mineral mapping on the Moon surface provides the clue to understand the origin, evolution, stratigra...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Science, 1974.I...
Present understanding of planetary composition is based primarily on remotely-sensed data, and in pa...
Reflectance spectra were computed for water ice and ammonia ice mixtures as functions of weight frac...
Here we present new laboratory spectral measurements of the major silicate minerals identified on th...
When a meteorite enters into the earth’s at-mosphere, it is immediately subjected to various chemica...
Diffuse reflectance spectra, 400-800 nm, were determined on minerals, goethite, hematite, ilmenite, ...
Supplemetary materials for the "Mapping the spectral and mineralogical variability of lunar breccia ...
Remote-sensing infrared spectroscopy is the principal field of investigation for planetary surfaces ...
A positive identification of the minerals olivine, plagioclase, and several types of pyroxenes were ...
We report the spectral reflectance of Martian meteorites from 0.3-2.6 microns for the purpose of cat...
Presented here are infrared reflectance spectra of a typical set of Apollo samples to illustrate spe...
The major mineralogical components of Yamato-791197 determined from reflectance spectra are calcium-...
For the last decade telescopic near infrared spectra have been obtained for small lunar areas. Such ...
Summary This dataset contains spectral reflectance values for laboratory mixtures that were created...
Mineral mapping on the Moon surface provides the clue to understand the origin, evolution, stratigra...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Science, 1974.I...
Present understanding of planetary composition is based primarily on remotely-sensed data, and in pa...
Reflectance spectra were computed for water ice and ammonia ice mixtures as functions of weight frac...
Here we present new laboratory spectral measurements of the major silicate minerals identified on th...
When a meteorite enters into the earth’s at-mosphere, it is immediately subjected to various chemica...
Diffuse reflectance spectra, 400-800 nm, were determined on minerals, goethite, hematite, ilmenite, ...
Supplemetary materials for the "Mapping the spectral and mineralogical variability of lunar breccia ...
Remote-sensing infrared spectroscopy is the principal field of investigation for planetary surfaces ...