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142 Nd Evidence for Early (>4.53 Ga) Global Differentiation of the Silicate Earth

Boyet, M., Carlson, R. W.·2005·Science

Abstract

New high-precision samarium-neodymium isotopic data for chondritic meteorites show that their 142 Nd/ 144 Nd ratio is 20 parts per million lower than that of most terrestrial rocks. This difference indicates that most (70 to 95%) of Earth's mantle is compositionally similar to the incompatible element–depleted source of mid-ocean ridge basalts, possibly as a result of a global differentiation 4.53 billion years ago (Ga), within 30 million years of Earth's formation. The complementary enriched reservoir has never been sampled and is probably located at the base of the mantle. These data influence models of Earth's compositional structure and require revision of the timing of global differentiation on Earth's Moon and Mars.

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Metadata

Authors
Boyet, M., & Carlson, R. W.
Venue
Science
Published
2005-07-22
Volume
309
Issue
5734
Pages
576-581
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1966022977
Cited by
643
References
2
FWCI
24.21
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: 142 Nd Evidence for Early (>4.53 Ga) Global Differentiation of the Silicate Earth. https://app.cochat.ai/papers/10.1126/science.1113634
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Boyet, M., & Carlson, R. W. (2005). 142 Nd Evidence for Early (>4.53 Ga) Global Differentiation of the Silicate Earth. Science. https://doi.org/10.1126/science.1113634

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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