Inverse Eigenvalue Problems for the Mantle
We represent the earth as a sphere with radius R and assume that the material is perfectly elastic and isotropic. Thus we ignore ellipticity, rotation, damping, lateral inhomogeneities and anisotropy.
KeywordsTravel Time Shear Wave Inverse Problem Lower Mantle Torsional Mode
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- Hald, O.H., Inverse eigenvalue problems for the mantle, II., Geophys. J. R. astr. Soc., to appear.Google Scholar