Three-dimensional structure of the Earth from splitting in free-oscillation spectra
Observations of splitting in free oscillations spectra can be used to constrain the three-dimensional distribution of heterogeneity in the Earth. Modes sampling mainly the Earth's mantle are compatible with the distributions of mantle heterogeneity inferred from P-wave travel times. The anomalo...
| Autors principals: | , , |
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| Format: | Journal article |
| Idioma: | English |
| Publicat: |
1987
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