High‐silica deposits of an aqueous origin in western Hellas Basin, Mars
Data from the Thermal Emission Spectrometer and the Thermal Emission Imaging System have been used to identify isolated high silica surfaces in western Hellas Basin. Deconvolution results indicate that the surfaces are composed of nearly 80% high silica phases (amorphous silica, phyllosilicates, or...
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| Hlavní autor: | |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Wiley
2008-06-01
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| Edice: | Geophysical Research Letters |
| Témata: | |
| On-line přístup: | https://doi.org/10.1029/2008GL033807 |
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