词条 | Palagonite |
释义 |
Palagonite soil is a light yellow-orange dust, comprising a mixture of particles ranging down to sub-micrometer sizes, usually found mixed with larger fragments of lava. The color is indicative of the presence of iron in the +3 oxidation state, embedded in an amorphous matrix. Palagonite tuff is a tuff composed of sideromelane fragments and coarser pieces of basaltic rock, embedded in a palagonite matrix. A composite of sideromelane aggregate in palagonite matrix is called hyaloclastite. Palagonite on MarsBased on infrared spectroscopy, the fine-grained component of Mauna-Kea palagonite is the terrestrial material with the best match to the spectral properties of Martian dust, and is believed to be similar in composition and in origin to dusty component of the surface regolith of Mars.[1][2] The palagonitic tephra from a cinder cone in Hawaii has been used to create Martian regolith simulant for researchers.[3] The spectroscopic signature of palagonitic alteration on Mars is used as evidence for the existence of water on Mars. References1. ^R.B. Singer, "Mineralogy of High-Albedo Soils and Dust on Mars", AGU paper 2B1214, J. Geophys. Res. 10, 159-10,168, 1982; also R. B. Singer and T. L. Roush, "Spectral reflectance properties of particulate weathered coatings on rocks: Laboratory modeling and applicability to Mars", in Lunar Plan. Sci. Conf. XIV, 708-709, 1983. 2. ^E.A. Guinness,R. E. Arvidson, M. A. Dale-Bannister, R. B. Singer and E. A. Brukenthal, "On the Spectral Reflectance Properties of Materials Exposed at the Viking Landing Sites", Proc. 17th Lunar and Planetary Science Conf., Part 2, J. Geophys. Res. 92, E575-E587, 1987. 3. ^{{cite book|title=JSC Mars-1: Martian regolith simulant|date=March 1997|publisher=Lunar and Planetary Exploration XXVIII|author=Allen, C. C.|author2=Morris, R. V.|author3=Lindstrom, D. J.|author4=Lindstrom, M. M.|author5=Lockwood, J. P.|url=http://www.orbitec.com/store/JSC_Mars_1_Characterization.pdf|accessdate=10 May 2014|deadurl=yes|archiveurl=https://web.archive.org/web/20140910011606/http://www.orbitec.com/store/JSC_Mars_1_Characterization.pdf|archivedate=10 September 2014|df=}}
3 : Igneous rocks|Volcanology|Glass in nature |
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