The inner inner core of the Earth: Texturing of iron crystals from three-dimensional seismic anisotropy

Xinlei Sun, Xiaodong Song

Research output: Contribution to journalArticlepeer-review

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 languageEnglish (US)
Pages (from-to)56-65
Number of pages10
JournalEarth and Planetary Science Letters
Volume269
Issue number1-2
DOIs
StatePublished - 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

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