Partitioning of nickel and cobalt between silicate perovskite and metal at pressures up to 80 GPa
about
Chemical interaction of Fe and Al(2)O3 as a source of heterogeneity at the Earth's core-mantle boundary.Partitioning experiments in the laser-heated diamond anvil cell: volatile content in the Earth's core.Structural change in molten basalt at deep mantle conditions.High-pressure experiments and the phase diagram of lower mantle and core materialsScrews tighten on the core
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Partitioning of nickel and cobalt between silicate perovskite and metal at pressures up to 80 GPa
description
article publié dans la revue scientifique Nature
@fr
scientific article published in Nature
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wetenschappelijk artikel
@nl
наукова стаття, опублікована в Nature у квітні 1999
@uk
name
Partitioning of nickel and cob ...... etal at pressures up to 80 GPa
@en
Partitioning of nickel and cob ...... etal at pressures up to 80 GPa
@nl
type
label
Partitioning of nickel and cob ...... etal at pressures up to 80 GPa
@en
Partitioning of nickel and cob ...... etal at pressures up to 80 GPa
@nl
prefLabel
Partitioning of nickel and cob ...... etal at pressures up to 80 GPa
@en
Partitioning of nickel and cob ...... etal at pressures up to 80 GPa
@nl
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Partitioning of nickel and cob ...... etal at pressures up to 80 GPa
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10.1038/19287
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1999-04-01T00:00:00Z
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1010045998