Shear-Wave Anisotropy in the Earth's Inner Core

Earth's inner core (IC) anisotropy is widely used to infer the deep Earth's evolution and present dynamics. Many compressional-wave anisotropy models have been proposed based on seismological observations. In contrast, inner-core shear-wave (J-wave) anisotropy-on a par with the compressional-wave anisotropy-has been elusive. Here, we present a new class of the J-wave anisotropy observations utilizing earthquake coda-correlation wavefield. We establish that the coda-correlation feature I2-J, sensitive to J-wave speed, exhibits time and amplitude changes when sampling the IC differently. J-waves traversing the IC near its center travel faster for the oblique than equatorial angles relative to the Earth's rotation axis by at least similar to 5 s. The simplest explanation is the J-wave cylindrical anisotropy with a minimum strength of similar to 0.8%, formed through the lattice-preferred-orientation mechanism of iron. Although we cannot uniquely determine its stable iron phase, the new observations rule out one of the body-centered-cubic iron models.

Automated summary

This study reveals a new class of J-wave anisotropy observations using earthquake coda-correlation wavefield, showing that J-waves traveling through the Earth's inner core exhibit speed differences due to cylindrical anisotropy possibly formed by the lattice-preferred-orientation mechanism of iron. These observations rule out one of the body-centered-cubic iron models, contributing to our understanding of deep Earth dynamics.