Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layer
The D$${}^{{\prime\prime} }$$ ″ layer in the Earth’s lower mantle involves a seismic discontinuity which is often assigned to a mineral phase transition to post-perovskite, however, as this phase transition occurs over broad region the assignment of seismic boundaries remains unclear. Here, the auth...
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2019-12-01
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Online Access: | https://doi.org/10.1038/s41467-019-13482-x |
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doaj-078c65dbb8b74458bdeab416a74032d22021-05-11T12:19:30ZengNature Publishing GroupNature Communications2041-17232019-12-011011910.1038/s41467-019-13482-xKinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layerChristopher Langrand0Denis Andrault1Stéphanie Durand2Zuzana Konôpková3Nadège Hilairet4Christine Thomas5Sébastien Merkel6Univ. Lille, CNRS, INRA, ENSCL, UMR 8207 - UMET - Unité Matériaux et TransformationsUniversité Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et VolcansInstitute of Geophysics, University of MünsterDESY Photon ScienceUniv. Lille, CNRS, INRA, ENSCL, UMR 8207 - UMET - Unité Matériaux et TransformationsInstitute of Geophysics, University of MünsterUniv. Lille, CNRS, INRA, ENSCL, UMR 8207 - UMET - Unité Matériaux et TransformationsThe D$${}^{{\prime\prime} }$$ ″ layer in the Earth’s lower mantle involves a seismic discontinuity which is often assigned to a mineral phase transition to post-perovskite, however, as this phase transition occurs over broad region the assignment of seismic boundaries remains unclear. Here, the authors find that due to the kinetics of the bridgmanite to post-perovskite transformation, thick transition layers can be detected by seismic reflections, unlike previously thought.https://doi.org/10.1038/s41467-019-13482-x |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Christopher Langrand Denis Andrault Stéphanie Durand Zuzana Konôpková Nadège Hilairet Christine Thomas Sébastien Merkel |
spellingShingle |
Christopher Langrand Denis Andrault Stéphanie Durand Zuzana Konôpková Nadège Hilairet Christine Thomas Sébastien Merkel Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layer Nature Communications |
author_facet |
Christopher Langrand Denis Andrault Stéphanie Durand Zuzana Konôpková Nadège Hilairet Christine Thomas Sébastien Merkel |
author_sort |
Christopher Langrand |
title |
Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layer |
title_short |
Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layer |
title_full |
Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layer |
title_fullStr |
Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layer |
title_full_unstemmed |
Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layer |
title_sort |
kinetics and detectability of the bridgmanite to post-perovskite transformation in the earth's d″ layer |
publisher |
Nature Publishing Group |
series |
Nature Communications |
issn |
2041-1723 |
publishDate |
2019-12-01 |
description |
The D$${}^{{\prime\prime} }$$ ″ layer in the Earth’s lower mantle involves a seismic discontinuity which is often assigned to a mineral phase transition to post-perovskite, however, as this phase transition occurs over broad region the assignment of seismic boundaries remains unclear. Here, the authors find that due to the kinetics of the bridgmanite to post-perovskite transformation, thick transition layers can be detected by seismic reflections, unlike previously thought. |
url |
https://doi.org/10.1038/s41467-019-13482-x |
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