Identifying dehydration-induced shear velocity anomaly in the Earth's core-mantle boundary.

ABSTRACT: The steep temperature gradient near the bottom of the mantle is known to generate a negative correlation between the shear wave velocity (V _S ) and the depth in most regions of the D″ layer, as detected by seismological observations. However, increasing V _S with depth is observed at the D″ layer beneath Central America, where the Farallon slab sinks, and the origin of this anomaly has not been well constrained. Here, we calculate the thermoelastic constants and obtain the elastic wave velocities of hydrous phase H with various Al contents and cation configurations, which may act as a water carrier to the D″ layer. We find its V _S to be substantially lower than the post-perovskite-type bridgmanite. The dehydration of

SUBMITTER: Han S 

PROVIDER: S-EPMC11764039 | biostudies-literature | 2025 Jan

REPOSITORIES: biostudies-literature