Abstract
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.
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References
Hald, O.H., Inverse eigenvalue problems for the mantle, Geophys. J. R. astr. Soc., 62 (1980), 41–48.
Hald, O.H., Inverse eigenvalue problems for the mantle, II., Geophys. J. R. astr. Soc., to appear.
Hochstadt, H. and Lieberman, B., An inverse Sturm-Liouville problem with mixed given data, SIAM J. appl. Math., 34 (1978), 676–680.
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© 1983 Birkhäuser Boston
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Hald, O.H. (1983). Inverse Eigenvalue Problems for the Mantle. In: Deuflhard, P., Hairer, E. (eds) Numerical Treatment of Inverse Problems in Differential and Integral Equations. Progress in Scientific Computing, vol 2. Birkhäuser Boston. https://doi.org/10.1007/978-1-4684-7324-7_10
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DOI: https://doi.org/10.1007/978-1-4684-7324-7_10
Publisher Name: Birkhäuser Boston
Print ISBN: 978-0-8176-3125-3
Online ISBN: 978-1-4684-7324-7
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