No Temporal Change Seen in High‐Frequency Waves Scattered Near the Core‐Mantle Boundary

Abstract The core‐mantle boundary (CMB) and the outermost core are dynamic and heterogeneous regions with time‐dependent flows. We examine two seismic raypaths, diffracted P and PKP precursors—both replete with scattering, with precisely repeating earthquakes. These earthquakes, occurring in the Sou...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Ruoyan Wang, John E. Vidale, Wei Wang
Format: Article
Language:English
Published: Wiley 2024-12-01
Subjects:
seismology
core
mantle
body wave
seismic array
repeating earthquakes
Online Access:https://doi.org/10.1029/2024GL112155

Internet

https://doi.org/10.1029/2024GL112155

Similar Items