A neon-E-rich phase in the Orgueil carbonaceous chondrite

Computer Science

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Carbonaceous Meteorites, Interstellar Matter, Meteoritic Composition, Neon Isotopes, Orgueil Meteorite, Geochemistry, Isotope Separation, Silicates, Trapped Particles

Scientific paper

Attention is given to a procedure for separating a silicate fraction which contains large amounts of neon-E from the carbonaceous chondrite Orgueil. In this fraction a 20Ne/22Ne ratio of 4.56 is measured. The obtained data support the hypothesis that neon-E might be associated with interstellar dust grains of the type not fully homogenized with the solar system and which retain some of their trapped neon. Neon results in a three-isotope diagram are presented.

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