Lithospheric anisotropy structure inferred from collocated teleseismic and magnetotelluric observations: Great Slave Lake shear zone, northern Canada
Accurate interpretation of SKS shear‐wave splitting observations requires inherently indeterminate depth information. Magnetotelluric electrical anisotropies are depth‐constrained, and thereby offer possible resolution of the SKS conundrum. MT and teleseismic instruments, deployed across the Great S...
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Veröffentlicht in: | Geophysical research letters 2004-10, Vol.31 (19), p.L19614.1-n/a |
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