Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D″ layer

Christopher Langrand, Denis Andrault, Stéphanie Durand, Zuzana Konôpková, Nadège Hilairet, Christine Thomas and Sébastien Merkel ()
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Christopher Langrand: Univ. Lille, CNRS, INRA, ENSCL, UMR 8207 - UMET - Unité Matériaux et Transformations
Denis Andrault: Université Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et Volcans
Stéphanie Durand: Institute of Geophysics, University of Münster
Zuzana Konôpková: DESY Photon Science
Nadège Hilairet: Univ. Lille, CNRS, INRA, ENSCL, UMR 8207 - UMET - Unité Matériaux et Transformations
Christine Thomas: Institute of Geophysics, University of Münster
Sébastien Merkel: Univ. Lille, CNRS, INRA, ENSCL, UMR 8207 - UMET - Unité Matériaux et Transformations

Nature Communications, 2019, vol. 10, issue 1, 1-9

Abstract: Abstract Bridgmanite, the dominant mineral in the Earth’s lower mantle, crystallizes in the perovskite structure and transforms into post-perovskite at conditions relevant for the D$${}^{{\prime\prime} }$$″ layer. This transformation affects the dynamics of the Earth’s lowermost mantle and can explain a range of seismic observations. The thickness over which the two phases coexist, however, can extend over 100 km, casting doubt on the assignment of the observed seismic boundaries. Here, experiments show that the bridgmanite to post-perovskite transition in (Mg$${}_{0.86}$$0.86,Fe$${}_{0.14}$$0.14)SiO$${}_{3}$$3 is fast on geological timescales. The transformation kinetics, however, affects reflection coefficients of $$P$$P and $$S$$S waves by more than one order of magnitude. Thick layers of coexisting bridgmanite and post-perovskite can hence be detected using seismic reflections. Morever, the detection and wave period dependence of D$${}^{{\prime\prime} }$$″ reflections can be used to constrain significant features of the Earth’s lowermost mantle, such as the thickness of the coexistence layer, and obtain information on temperature and grain sizes.

Date: 2019
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DOI: 10.1038/s41467-019-13482-x

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