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Theoretical and experimental evidence for a post-perovskite phase of MgSiO3 in Earth's D″ layer

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Oganov, Artem R., Ono, Shigeaki·2004·Nature

Abstract

The Earth's lower mantle is believed to be composed mainly of (Mg,Fe)SiO3 perovskite, with lesser amounts of (Mg,Fe)O and CaSiO3 (ref. 1). But it has not been possible to explain many unusual properties of the lowermost ∼150 km of the mantle (the D″ layer) with this mineralogy. Here, using ab initio simulations and high-pressure experiments, we show that at pressures and temperatures of the D″ layer, MgSiO3 transforms from perovskite into a layered CaIrO3-type post-perovskite phase. The elastic properties of the post-perovskite phase and its stability field explain several observed puzzling properties of the D″ layer: its seismic anisotropy, the strongly undulating shear-wave discontinuity at its top and possibly the anticorrelation between shear and bulk sound velocities.

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Metadata

Authors
Oganov, A. R., & Ono, S.
Venue
Nature
Published
2004-07
Volume
430
Issue
6998
Pages
445-448
ISSN
  • 0028-0836 (ISSN-L)
  • 1476-4687
OpenAlex
W1970101802
Cited by
1,000
References
3
FWCI
62.84
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: Theoretical and experimental evidence for a post-perovskite phase of MgSiO3 in Earth's D″ layer. https://app.cochat.ai/papers/10.1038/nature02701
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Oganov, A. R., & Ono, S. (2004). Theoretical and experimental evidence for a post-perovskite phase of MgSiO3 in Earth's D″ layer. Nature. https://doi.org/10.1038/nature02701

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

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.