Widespread Deformation at the Base of the Mantle Linked to Subducted Slabs
In Earth’s deepest mantle (D″), shear wave speeds can vary with propagation and vibration direction of the wave because of convection-driven mantle deformation, a phenomenon known as seismic anisotropy. Although D″ anisotropy has been mapped globally at long wavelengths (>4000 km laterally) in tomog...
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| Hlavní autoři: | , , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Seismological Society of America
2026-04-01
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| Edice: | The Seismic Record |
| On-line přístup: | https://doi.org/10.1785/0320260001 |
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