Seismic evidence for a 1000 km mantle discontinuity under the Pacific
This study uses reverse-time migration full-waveform seismic imaging to reveal a thinned transition zone and a 1000-km mid-mantle discontinuity under the Pacific near Hawaii which they link to the upper boundary of upwelling plume material.
| Váldodahkkit: | , , , |
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| Materiálatiipa: | Artihkal |
| Giella: | English |
| Almmustuhtton: |
Nature Portfolio
2023-03-01
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| Ráidu: | Nature Communications |
| Liŋkkat: | https://doi.org/10.1038/s41467-023-37067-x |