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Mantle structure slice - PowerPoint PPT Presentation

Rayleigh wave group velocity maps

Rayleigh wave group velocity maps. At short periods, group velocities are slow because of the thick, slow crust At long periods, group velocities are neutral to fast because the crust is compensated by fast material in the upper mantle. Low-velocity uppermost mantle beneath North-Central Tibet.

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Rayleigh wave group velocity maps