1887

Abstract

Interpretation of TDEM sounding data is commonly done using the S-layer differential transform. This method is<br>based on the thin sheet model. In this method, the first and second time derivates of the magnetic field are solved<br>simultaneously for the conductance (S) and depth (d). Taking the derivatives of S to d then yields the conductivity<br>of an equivalent S-layer and depth d.

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/content/papers/10.3997/2214-4609-pdb.154.041
2005-09-14
2022-05-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.154.041
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