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

NATURE, no. 7307 (2010): 744-U9

Cited: 95|Views22

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pubmed.ncbi.nlm.nih.gov academic.microsoft.com arxiv.org

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Geology Geophysics Planetary sciences Earth sciences

Abstract

In addition to its global North-South anisotropy(1), there are two other enigmatic seismological observations related to the Earth's inner core: asymmetry between its eastern and western hemispheres(2-6) and the presence of a layer of reduced seismic velocity at the base of the outer core(6-12). This 250-km-thick layer has been interprete...More

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Thierry Alboussière

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Renaud Deguen

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Mickaël Melzani

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