Hydrothermal formation of Clay-Carbonate alteration assemblages in the Nili Fossae region of Mars

The Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) has returned observations of the Nili Fossae region indicating the presence of Mg-carbonate in small (< 10 km sq 2), relatively bright rock units that are commonly fractured (Ehlmann et al., 2008b). We have analyzed spectra from CRI...

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Bibliographic Details
Published in:Earth and planetary science letters 2010-08, Vol.297 (1), p.174-182
Main Authors: Brown, Adrian J., Hook, Simon J., Baldridge, Alice M., Crowley, James K., Bridges, Nathan T., Thomson, Bradley J., Marion, Giles M., de Souza Filho, Carlos R., Bishop, Janice L.
Format: Article
Language:English
Subjects:
Alterations
carbonate
Carbonates
clay-carbonate alteration
CRISM
Earth
Geology
Mars
Minerals
Nili Fossae
Rock
Spectra
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Summary:The Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) has returned observations of the Nili Fossae region indicating the presence of Mg-carbonate in small (< 10 km sq 2), relatively bright rock units that are commonly fractured (Ehlmann et al., 2008b). We have analyzed spectra from CRISM images and used co-located HiRISE images in order to further characterize these carbonate-bearing units. We applied absorption band mapping techniques to investigate a range of possible phyllosilicate and carbonate minerals that could be present in the Nili Fossae region. We also describe a clay-carbonate hydrothermal alteration mineral assemblage in the Archean Warrawoona Group of Western Australia that is a potential Earth analog to the Nili Fossae carbonate-bearing rock units. We discuss the geological and biological implications for hydrothermal processes on Noachian Mars.
ISSN:0012-821X
1385-013X
DOI:10.1016/j.epsl.2010.06.018