Low viscosity of the Earth’s inner core
The inner core of the Earth is formed of a crystalline solid which is mostly composed of iron. Here, the authors use molecular dynamics methods to show that the crystalline structure of the inner core may have a viscosity close to that of liquid iron, despite being a solid.
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Nature Publishing Group
2019-06-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-019-10346-2 |