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    Terrestrial analogues of the surface rocks of Mars? (1986)
    [s.l.] : Nature Publishing Group
    Nature 320 (1986), S. 55-56 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The red colour of the surface of Mars has long been attributed to Fe3+-bearing minerals in the regolith, implying that oxidizing conditions have prevailed. However, the apparent enrichment of iron in martian regolith, its mineralogy and the nature of the unweathered parent rocks remain poorly ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/320055a0
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