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Planetary science

Earth's building blocks

Nature volume 541, pages 468–469 (2017)Cite this article

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Earth grew by the accretion of meteoritic material. High-precision isotopic data reveal how the composition of this material changed over time, forcing revision of models of our planet's formation. See Letters p.521 & p.525

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Figure 1: Probing Earth's formation.

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Authors and Affiliations

  1. Richard W. Carlson is in the Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington DC 20015, USA.,

    Richard W. Carlson

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  1. Richard W. Carlson
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Correspondence to Richard W. Carlson.

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Carlson, R. Earth's building blocks. Nature 541, 468–469 (2017). https://doi.org/10.1038/541468a

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