Abstract
The gray crystalline hematite at Meridiani Planum first discovered by the Mars Global Surveyor Thermal Emission Spectrometer (MGS-TES) instrument occurs as spherules that have been interpreted as concretions. Analysis of the TES and mini-TES spectra shows that no 390 cm-1 feature is present in the characteristic martian hematite spectrum. Here, we incorporate the mid-IR optical constants of hematite into a simple Fresnel reflectance model to understand the effect of emission angle and crystal morphology on the presence or absence of the 390 cm-1 feature in an IR hematite spectrum. Based on the results we offer two models for the internal structure of the martian hematite spherules.
Original language | English (US) |
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Pages (from-to) | 408-418 |
Number of pages | 11 |
Journal | Icarus |
Volume | 181 |
Issue number | 2 |
DOIs | |
State | Published - Apr 2006 |
Keywords
- Infrared observations
- Mars, surface
- Mineralogy
- Spectroscopy
ASJC Scopus subject areas
- Astronomy and Astrophysics
- Space and Planetary Science