Density structure of Earth's lowermost mantle from Stoneley mode splitting observations
Advances in our understanding of Earth’s thermal evolution and the style of mantle convection rely on robust seismological constraints on lateral variations of density. The largelow-shear-wave velocity provinces (LLSVPs) atop the core-mantle boundary beneath Africa and the Pacific are the largest st...
| Príomhchruthaitheoirí: | , , |
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| Formáid: | Journal article |
| Foilsithe / Cruthaithe: |
Springer Nature
2017
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