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
Hauptverfasser: Waite, Gregory P., Smith, Robert B., Allen, Richard M.
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Sprache:eng
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