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- W1786475863 abstract "This chapter discusses the inverse problems in modern magnetotellurics. The inverse problem in modern magnetotellurics using the plane-wave approximation of the source field consists in the determination of the geoelectric structure of the Earth from a known dependence of magnetotelluric (MT) and magnetovariational (MV) response functions on the observation coordinates x,y,z = 0, and the frequency of the electromagnetic field. When solving the multi-dimensional inverse problem, one can face a contradiction between a finite area of MT and MV observations and a mathematical statement calling for conditions at infinity. Strategy and informativeness of the inverse problems depend on the dimensionality of models in use. The simple inverse problem is 1-D inversion carried out in the class of 1-D models. It applies the mathematics of zero horizontal derivatives. Such mathematics provides the local determination of the electrical conductivity along vertical profiles passing through observation points." @default.
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- W1786475863 date "2006-01-01" @default.
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- W1786475863 title "Chapter 7 Inverse Problems in Modern Magnetotellurics" @default.
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- W1786475863 doi "https://doi.org/10.1016/s0076-6895(06)40007-x" @default.
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