Lithospheric Structure Across the Northern Canadian Cordillera from Teleseismic Receiver Functions
A major change in seismic velocities between Earth’s crust and mantle is known as the Mohorovicic discontinuity (Moho). The depth of the Moho plays an important role in characterizing the overall structure of the crust and can be related to the tectonic setting of a region. Teleseismic P-wave receiv...
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| Language: | en |
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Université d'Ottawa / University of Ottawa
2016
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| Online Access: | http://hdl.handle.net/10393/35535 http://dx.doi.org/10.20381/ruor-493 |