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Titlebook: Astromineralogy; Thomas Henning Book 2010Latest edition Springer-Verlag Berlin Heidelberg 2010 Accretion.Casini cosmic dust analyser.Spitz

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Die Forschung selbst nachhaltig gestaltento ~200 ppm..Isotope abundance anomalies are the key feature based on which the presolar nature of a given grain is ascertained. They also allow identifying likely stellar sources for the grains. The major source of SiC, the oxide and the silicate grains are Red Giant/AGB stars, while some (~1%) of
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The Mineralogy of Interstellar and Circumstellar Dust in Galaxies,environment in which it is found. Dust can therefore be used as a tracer and probe of the physical and chemical conditions where it is detected. We present an observational overview of interstellar and circumstellar dust using spectroscopy at infrared wavelengths. Thanks to the contributions made by
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The Mineralogy of Cometary Dust, other minerals. While forsterite Mg.SiO. and enstatite MgSiO. are the most common silicate minerals, both the olivine and pyroxenes also show a wide range in Mg/Fe in at least some comets. Carbon in the dust is enriched relative to CI chondrites; a significant fraction of the carbon is in the form
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The Astromineralogy of Interplanetary Dust Particles,beyond the giant planets, presolar grains or “astrominerals” with solar and non-solar isotopic compositions are expected to be even more abundant in cometary IDPs than in primitive meteorites. Non-solar D/H and .N/.N isotopic enrichments in chondritic IDPs are associated with a carbonaceous carrier.
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The Most Primitive Material in Meteorites,er phases of isotopically anomalous noble gases and isolated from the bulk meteorites using harsh chemical treatments. Diamond was the first and may occur with an abundance ‾1‰, but it is not clear what fraction of the observed nanometer-sized diamonds is truly presolar. Others found by this approac
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