East European sedimentary basins long heated by a fading mantle upwelling
Abstract A strong negative anomaly of seismic wave velocities at the core-mantle boundary (the Perm Anomaly) beneath the East European platform is attributed to the remnant of a deep mantle upwelling. The interaction between the upwelling and the East European lithosphere in the geological past and...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2024-05-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-024-48127-1 |