Analysis of lunar pyroclastic deposit FeO abundances by LRO Diviner
[1] Thermal infrared reflectance spectra of rock‐forming minerals include a prominent minimum near 8μm, known as the “Christiansen feature” (CF). The inflection point wavelength is sensitive to the degree of polymerization of silicates, which is strongly influenced by major cations – notably iron –...
| Main Authors: | , , , |
|---|---|
| Format: | Journal article |
| Published: |
American Geophysical Union
2012
|