Regional variation of inner core anisotropy from seismic normal mode observations.
Earth's solid inner core is surrounded by a convecting liquid outer core, creating the geodynamo driving the planet's magnetic field. Seismic studies using compressional body waves suggest hemispherical variation in the anisotropic structure of the inner core, but are poorly constrained be...
| Main Authors: | , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2010
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