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...

Full description

Bibliographic Details
Main Authors: Christopher Langrand, Denis Andrault, Stéphanie Durand, Zuzana Konôpková, Nadège Hilairet, Christine Thomas, Sébastien Merkel
Format: Article
Language:English
Published: Nature Publishing Group 2019-12-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-019-13482-x
id doaj-078c65dbb8b74458bdeab416a74032d2
record_format Article
spelling 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
work_keys_str_mv AT christopherlangrand kineticsanddetectabilityofthebridgmanitetopostperovskitetransformationintheearthsdlayer
AT denisandrault kineticsanddetectabilityofthebridgmanitetopostperovskitetransformationintheearthsdlayer
AT stephaniedurand kineticsanddetectabilityofthebridgmanitetopostperovskitetransformationintheearthsdlayer
AT zuzanakonopkova kineticsanddetectabilityofthebridgmanitetopostperovskitetransformationintheearthsdlayer
AT nadegehilairet kineticsanddetectabilityofthebridgmanitetopostperovskitetransformationintheearthsdlayer
AT christinethomas kineticsanddetectabilityofthebridgmanitetopostperovskitetransformationintheearthsdlayer
AT sebastienmerkel kineticsanddetectabilityofthebridgmanitetopostperovskitetransformationintheearthsdlayer
_version_ 1721445000037793792