Dislocation creep may control bridgmanite deformation in the Earth’s lower mantle
Abstract Seismic anisotropy in the Earth’s lower mantle, particularly around subduction zones, is commonly attributed to deformation by dislocation creep, yet much of the lower mantle appears nearly isotropic. This contrast complicates interpretations of mantle rheology. Here we report the temperatu...
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| Váldodahkkit: | , , , , , , |
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| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Nature Portfolio
2026-01-01
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| Ráidu: | Communications Earth & Environment |
| Liŋkkat: | https://doi.org/10.1038/s43247-026-03212-9 |
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