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Abstract

In this presentation we show that the interpretation of spatial densely sampled TEM data over 2D<br>earth structures is greatly enhanced by inverting the data using the 1D-LCI algorithm (Laterally<br>Constrained Inversion). In the 1D-LCI algorithm neighboring models are constrained laterally on layer<br>resistivities and interfaces.

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/content/papers/10.3997/2214-4609-pdb.183.514-518
2005-04-03
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.183.514-518
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