The elastic properties and stability of fcc-Fe and fcc-FeNi alloys at inner-core conditions
The agreement between shear wave velocities for the Earth's inner core observed from seismology with those derived from mineral physics is considerably worse than for any other region of the Earth. Furthermore, there is still debate as to the phase of iron present in the inner core, particularl...
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| Veröffentlicht in: | Geophysical journal international 2015-07, Vol.202 (1), p.94-101 |
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| Hauptverfasser: | , , , |
| Format: | Artikel |
| Sprache: | eng |
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