том 430 издание 6998 страницы 445-448

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

Тип публикацииJournal Article
Дата публикации2004-07-21
scimago Q1
wos Q1
white level БС1
SJR18.288
CiteScore78.1
Impact factor48.5
ISSN00280836, 14764687
Multidisciplinary
Краткое описание
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 anisotropy2, the strongly undulating shear-wave discontinuity at its top3,4,5,6 and possibly the anticorrelation between shear and bulk sound velocities7,8.
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ГОСТ |
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Oganov A. R., Ono S. Theoretical and experimental evidence for a post-perovskite phase of MgSiO3 in Earth's D″ layer // Nature. 2004. Vol. 430. No. 6998. pp. 445-448.
ГОСТ со всеми авторами (до 50) Скопировать
Oganov A. R., Ono S. Theoretical and experimental evidence for a post-perovskite phase of MgSiO3 in Earth's D″ layer // Nature. 2004. Vol. 430. No. 6998. pp. 445-448.
RIS |
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TY - JOUR
DO - 10.1038/nature02701
UR - https://doi.org/10.1038/nature02701
TI - Theoretical and experimental evidence for a post-perovskite phase of MgSiO3 in Earth's D″ layer
T2 - Nature
AU - Oganov, Artem R.
AU - Ono, Shigeaki
PY - 2004
DA - 2004/07/21
PB - Springer Nature
SP - 445-448
IS - 6998
VL - 430
PMID - 15269766
SN - 0028-0836
SN - 1476-4687
ER -
BibTex |
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BibTex (до 50 авторов) Скопировать
@article{2004_Oganov,
author = {Artem R. Oganov and Shigeaki Ono},
title = {Theoretical and experimental evidence for a post-perovskite phase of MgSiO3 in Earth's D″ layer},
journal = {Nature},
year = {2004},
volume = {430},
publisher = {Springer Nature},
month = {jul},
url = {https://doi.org/10.1038/nature02701},
number = {6998},
pages = {445--448},
doi = {10.1038/nature02701}
}
MLA
Цитировать
Oganov, Artem R., and Shigeaki Ono. “Theoretical and experimental evidence for a post-perovskite phase of MgSiO3 in Earth's D″ layer.” Nature, vol. 430, no. 6998, Jul. 2004, pp. 445-448. https://doi.org/10.1038/nature02701.
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