Spectral analysis of magnetic anomalies over the area of NW Poland southwest of the Teisseyre-Tornquist Line has been carried out in an effort to estimate the depth to magnetic sources. Average magnetic source depth of 18.5 km has been obtained for the area and this is thought to be related to the depth to the top of the main anomalous structures in the area. This value coincides with the depth to the top of the crystalline crust determined from seismic data.
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