| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 10701496 | Icarus | 2011 | 30 Pages |
Abstract
⺠Most CI reflectance spectra exhibit mineral-associated absorption bands. ⺠Magnetite seems the likeliest explanation for blue-sloped CI spectra. ⺠Larger grain size samples generally have the bluest and darkest spectra. ⺠Phase angle can cause CI spectra to become redder or bluer. ⺠Underdense CI samples have lower reflectance than regularly packed CI samples.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Space and Planetary Science
Authors
E.A. Cloutis, T. Hiroi, M.J. Gaffey, C.M.O'D. Alexander, P. Mann,