title: High-Pressure Elasticity of Iron and Anisotropy of Earth's Inner Core.
abstract: A first principles theoretical approach shows that, at the density of the inner core, both hexagonal [hexagonal close-packed (hcp)] and cubic [face-centered-cubic (fcc)] phases of iron are substantially elastically anisotropic. A forward model of the inner core based on the predicted elastic constants and the assumption that the inner core consists of a nearly perfectly aligned aggregate of hcp crystals shows good agreement with seismic travel time anomalies that have been attributed to inner core anisotropy. A cylindrically averaged aggregate of fcc crystals disagrees with the seismic observations.
authors.forename: L
authors.initials: L
authors.lastname: Stixrude
authors.forename: R E
authors.initials: RE
authors.lastname: Cohen