Mantle provinces under North America from multifrequency P wave tomography
This is a survey of mantle provinces (large-scale seismic anomalies) under North America, from the surface down to 1500-1800 km depth. The underlying P velocity model was obtained by multifrequency tomography, a waveform-based method that systematically measures and models the frequency-dependence o...
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| Format: | Journal article |
| Language: | English |
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American Geophysical Union
2011
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