Crust-mantle decoupling revealed by seismic velocity anisotropy beneath Syowa Station, Antarctica
We analyzed shear wave splittings in the crust beneath Syowa Station, using Moho converted Ps waves. Three set of receiver functions and stacked receiver functions from Tonga events are analyzed. Results are interpreted by conbining with seismic anisotropy in the mantle, which have been revealed by...
| Main Authors: | , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
National Institute of Polar Research
1997-07-01
|
| Series: | Antarctic Record |
| Online Access: | http://doi.org/10.15094/00009000 |