Abstract
We present a three-dimensional model of the seismic anisotropy and texturing of iron crystals in the inner core. The form of the anisotropy changes suddenly at slightly less than half of the inner core radius. The outer part is composed of iron crystals of a single phase with different degrees of preferred alignment along the spin axis of the Earth. The inner part may be composed of a different phase of crystalline iron or have a different pattern of alignment.
Original language | English (US) |
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Pages (from-to) | 56-65 |
Number of pages | 10 |
Journal | Earth and Planetary Science Letters |
Volume | 269 |
Issue number | 1-2 |
DOIs | |
State | Published - May 15 2008 |
Keywords
- inner core anisotropy
- inner inner core
- iron alignment
- seismic waves
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science