Spectroscopic Identification of Carbonate Minerals in the Martian Dust

Author:

Bandfield Joshua L.1,Glotch Timothy D.1,Christensen Philip R.1

Affiliation:

1. Department of Geological Sciences, Arizona State University, Tempe, AZ 85287–6305, USA.

Abstract

Thermal infrared spectra of the martian surface indicate the presence of small concentrations (∼2 to 5 weight %) of carbonates, specifically dominated by magnesite (MgCO 3 ). The carbonates are widely distributed in the martian dust, and there is no indication of a concentrated source. The presence of small concentrations of carbonate minerals in the surface dust and in martian meteorites can sequester several bars of atmospheric carbon dioxide and may have been an important sink for a thicker carbon dioxide atmosphere in the martian past.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference33 articles.

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5. S. J. Gaffeyet al., in Remote Geochemical Analysis: Elemental and Mineralogical Composition, C. M. Pieters, P. Englert, Eds. (Cambridge Univ. Press, New York, 1993), pp. 43–71.

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