Approximate sensitivities for the multi-dimensional electromagnetic inverse problem
Inversion of measurements from a geophysical electromagnetic survey to produce a two- or three-dimensional conductivity model of the Earth is computationally demanding. The classical approach is to linearise the inverse problem and iterate towards the solution. A typical, modern version of this a...
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| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/2429/7282 |