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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主要作者: Sigloch, K
格式: Journal article
语言:English
出版: American Geophysical Union 2011

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