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Melting-induced stratification above the Earth’s inner core due to convective translation

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  • Thierry Alboussière

    (Laboratoire de Géophysique Interne et Tectonophysique, CNRS, Observatoire de Grenoble, Université Joseph Fourier, Maison des Géosciences, BP 53, 38041 Grenoble Cedex 9, France
    Université de Lyon, CNRS UMR5570, site UCB Lyon 1, 2 rue Raphaël Dubois, bâtiment Géode, 69622 Villeurbanne, Université Lyon 1)

  • Renaud Deguen

    (Laboratoire de Géophysique Interne et Tectonophysique, CNRS, Observatoire de Grenoble, Université Joseph Fourier, Maison des Géosciences, BP 53, 38041 Grenoble Cedex 9, France
    Johns Hopkins University)

  • Mickaël Melzani

    (Laboratoire de Géophysique Interne et Tectonophysique, CNRS, Observatoire de Grenoble, Université Joseph Fourier, Maison des Géosciences, BP 53, 38041 Grenoble Cedex 9, France)

Abstract

Melting-induced core anomalies Several observed properties of Earth's solid inner core and liquid outer core remain enigmatic, including an east–west seismic asymmetry and the presence of a roughly 250-kilometre-thick layer of reduced seismic velocity at the base of the outer core. Alboussière et al. now suggest a model that can produce both of these features. Based on experiment and numerical modelling, they propose that simultaneous crystallization and melting at opposite sides of Earth's inner-core surface can result in a translational mode of thermal convection within the inner core, which also introduces an asymmetry between hemispheres.

Suggested Citation

  • Thierry Alboussière & Renaud Deguen & Mickaël Melzani, 2010. "Melting-induced stratification above the Earth’s inner core due to convective translation," Nature, Nature, vol. 466(7307), pages 744-747, August.
  • Handle: RePEc:nat:nature:v:466:y:2010:i:7307:d:10.1038_nature09257
    DOI: 10.1038/nature09257
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    Cited by:

    1. Shichuan Sun & Yu He & Junyi Yang & Yufeng Lin & Jinfeng Li & Duck Young Kim & Heping Li & Ho-kwang Mao, 2023. "Superionic effect and anisotropic texture in Earth’s inner core driven by geomagnetic field," Nature Communications, Nature, vol. 14(1), pages 1-8, December.

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