Significance of the terrestrial Mg/Si ratio

Computer Science

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Asteroid Belts, Carbonaceous Chondrites, Halley'S Comet, Interplanetary Dust, Magnesium, Silicon, Chemical Composition, Earth Mantle, Solar System, Terrestrial Planets

Scientific paper

The results of Rietmeijer's (1988) comparison of the compositions of chondritic interplanetary dust particles with the composition of C1 chondrites is examined. Rietmeijer concluded that there has been a radial chemical differentiation between the two source regions in the inner and outer solar system. The assumption that the Mg/Si ratio of C1 chondrites is representative of the sun and the primitvie solar nebula is evaluated. Evidence bearing upon the Mg/Si ratios of planetary bodies in the inner solar system are reviewed. Data are included for Venus, the moon, Mars, S-type asteroids, and the eucrite parent bodies. It is found that these bodies are generally dominanted by mineralogies with Mg/Si ratios substantially higher than the C1 chondritic value. This regional Mg/Si ratio is shown to be consistent with the solar ratio, within experimental uncertainties.

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