Inner core anisotropy measured using new ultra-polar PKIKP paths
We measure the seismic anisotropy of the inner core using PKPbc-PKPdf and PKPab-PKPdf differential traveltimes, as a function of the angle ζ between the Earth’s rotation axis and the ray path in the inner core. Previous research relied heavily on body waves originating in the South Sandwich Islands...
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Language: | English |
Published: |
2020
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Online Access: | https://dspace.library.uu.nl/handle/1874/411203 |