VP and VS structure of the Yellowstone hot spot from teleseismic tomography: Evidence for an upper mantle plume
The movement of the lithosphere over a stationary mantle magmatic source, often thought to be a mantle plume, explains key features of the 16 Ma Yellowstone–Snake River Plain volcanic system. However, the seismic signature of a Yellowstone plume has remained elusive because of the lack of adequate d...
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Veröffentlicht in: | Journal of Geophysical Research. B. Solid Earth 2006-04, Vol.111 (B4), p.n/a |
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