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PREM has been widely used as the basis for [[seismic tomography]] and related global [[geophysics|geophysical]] models. PREM incorporates anelastic dispersion and [[seismic anisotropy|anisotropy]] and therefore it is frequency-dependent and transversely isotropic for the [[Mantle (geology)|upper mantle]].
PREM
PREM was developed by [[Adam Dziewonski|Adam M. Dziewonski]] and [[Don L. Anderson]].
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