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- W2149742009 abstract "The presence of seismic anisotropy in the oceanic crust and upper mantle has been detected. Associated electrical anisotropy may be present. Anisotropy is introduced into Maxwell's equations through the conductivity and permittivity. The resulting partial differential equations can be decoupled into separate transverse magnetic (TM) and poloidal magnetic (PM) equations only if the conductivity and permittivity are axially symmetric, i.e. are transversely isotropic. The TM and PM modes do not decouple for transverse anisotropy. The electromagnetic response of a transversely anisotropic earth can be computed by using, for example, an integral equation approach. The integral equation method is easily modified to include anisotropy." @default.
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- W2149742009 date "1986-05-01" @default.
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- W2149742009 title "The inclusion of anisotropy in Maxwell's equations" @default.
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- W2149742009 doi "https://doi.org/10.1111/j.1365-246x.1986.tb04539.x" @default.
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