Abstract
A thin conducting plate has proven to be a versatile model indescribing various relevant geologic features in crystallinebedrock. During the last few years we have developed severalinversion codes for some commonly used electromagnetic (EM)measurements that are based on this model. Both when developingand when applying inversion codes, it is necessary to have a goodunderstanding of how the properties of the model parametersaffect the model response. We have studied the parameters ofthe plate model by using the misfit mapping technique and singularvalue decomposition. These studies include both time andfrequency domain EM systems. We highlight the majordifferences between a plate model in free space and inconductive surroundings.
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