A008 LATERALLY CONSTRAINED 1D-INVERSION OF 3D TEM DATA Summary 1 In this presentation we show that the interpretation of spatial densely sampled TEM data over 2D earth structures is greatly enhanced by inverting the data using the 1D-LCI algorithm (Laterally Constrained Inversion). In the 1D-LCI algorithm neighboring models are constrained laterally on layer resistivities and interfaces. Introduction E. AUKEN A. V. CHRISTIANSEN L. JACOBSEN AND K. I. SØRENSEN The HydroGeophysics Group Department of Earth Sciences University of Aarhus Denmark Finlandsgade 8 8200 Århus N Transient EM (TEM) is commonly used in hydrogeophysical investigations as a fast and relatively cheap method


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