The Hilbert transform of the magnetic anomalies and the application in Inner Mongolia somewhere

Usually, the field measurements of magnetic prospecting is only observed for a parameter, the data obtained is relatively simple, as the multiple solutions of the geophysical interpretation, it increased the difficulty to the interpretation in complex geological conditions^[1]. This paper mainly discusses the use of Hilbert transform method calculated with the conversion between magnetic anomaly T, Z and H, eninch the data content, enhance the accuracy of the interpretation. Theoretical model and the actual Data Interpretation of Inner work proved the accuracy and effectiveness of the method.