The formation of Mg,Fe-silicates by reactions between amorphous magnesiosilica smoke particles and metallic iron nanograins with implications for comet silicate origins

Author:

Rietmeijer Frans J. M.1,Nuth Joseph A.2,Pun Aurora1

Affiliation:

1. Department of Earth and Planetary Sciences; 1-University of New Mexico; MSC3-2040 Albuquerque New Mexico 87131-0001 USA

2. Astrochemistry Laboratory, Solar System Exploration Division; NASA Goddard Space Flight Center; Code 691 Greenbelt Maryland 20771 USA

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Reference66 articles.

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2. Phase evolution in Fe2O3/MgO nanocomposite prepared via a simple precipitation method;Azhari;Materials Chemistry and Physics,2010

3. The dehydration of brucite;Ball;Mineralogical Magazine,1961

4. Elemental abundances in Leonid and Perseid meteoroids;Borovička;Earth, Moon, and Planets,2004

5. Processing of silicate dust grains in Herbig Ae/Be systems;Bouwman;Astronomy & Astrophysics,2001

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