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• W2065430131 abstract "Significance Understanding volatile elements in the early solar system is a key step toward understanding the processes of planetary formation and the composition of Earth, but the origin of volatiles on Earth is not well understood. In this article, we present measurements of silicon isotope ratios in angrites, a class of meteorites dating from the first few million years after condensation of solids from the solar nebula. We show that the silicon isotope composition of angrites is consistent with a depletion of volatile elements on the angrite parent body through impact events during accretion. Such volatile-poor planetesimals may represent the material that formed the Earth." @default.
• W2065430131 created "2016-06-24" @default.
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• W2065430131 date "2014-11-17" @default.
• W2065430131 modified "2023-10-16" @default.
• W2065430131 title "Silicon isotopes in angrites and volatile loss in planetesimals" @default.
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• W2065430131 doi "https://doi.org/10.1073/pnas.1418889111" @default.
• W2065430131 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/4260610" @default.
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• W2065430131 hasPublicationYear "2014" @default.
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