Abstract:The inversion of magnetic data to characterize dyke swarms is a challenging problem due to complexity of the anomalies arisen from multiple sources in different depth levels and with variable magnetic properties. It makes difficult to account for the number of dyke unities along a profile as well as unambiguous estimates about position, depth to the top and magnetization properties for single unities.We develop a procedure to obtain mean properties for juxtaposed dykes by using non-linear data inversion for th… Show more
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