作者: S. C. Kirkwood
DOI: 10.1111/J.1365-246X.1978.TB04752.X
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摘要: Summary. The limitations of isotropic modelling in the inversion anisotropic surface-wave phase velocities are examined. Inversion synthetic dispersion data for some model ocean-basin structures is used to demonstrate that inversions can give inaccurate and misleading estimates upper-mantle properties when anisotropy present.