Analysis of geomagnetic depth sounding data
The electromagnetic induction problem is non-linear, and thus is very difficult to solve for all but the simplest symmetries. Because of this, quantitative modelling of the conductivity structure from geomagnetic depth sounding data is expensive and time consuming, and the possibility that the anoma...
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| Language: | English |
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2010
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| Online Access: | http://hdl.handle.net/2429/22546 |