Dʺ structures beneath the East China Sea resolved by P‐wave slowness anomalies
The Dʺ layer, defined as 200–400 km in the lowermost mantle, is a thermal and chemical
boundary layer between the solid silicate mantle and the liquid outer core. Deciphering the …
boundary layer between the solid silicate mantle and the liquid outer core. Deciphering the …
Localized ultra‐low velocity zone as a strong scatterer at the core‐mantle boundary beneath central America
Small‐scale scatterers in the lower mantle contain key information on the recycling process
in the whole mantle. Resolving the fine structures of these scatterers is crucial for …
in the whole mantle. Resolving the fine structures of these scatterers is crucial for …
[HTML][HTML] The Use of Azimuthal Variation in ScS–S Differential Travel Times to Investigate Possible Anisotropy in the Lowermost Mantle Beneath the Philippines
S Tanaka - Geosciences, 2025 - mdpi.com
We collected approximately 500 ScS–S differential travel times passing beneath the
Philippines with various azimuths to discuss whether there were azimuthal variations in the …
Philippines with various azimuths to discuss whether there were azimuthal variations in the …