کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4740480 | 1641163 | 2013 | 4 صفحه PDF | دانلود رایگان |

We presented a new method for interpreting 2D magnetic data, called direct analytic signal (DAS) method, which directly used the analytic signal of magnetic anomaly to compute the depth and the structural index of the source. The DAS method needs only the computation of the first order derivatives of magnetic anomaly, so that the inversion results are more stable than the results obtained by the other existing analytic signal methods. The DAS method is tested on synthetic magnetic data with and without noise, and the DAS method can successfully obtain the depth and the structural index of the source. We also applied the DAS method to interpret a real magnetic data over a shallow geological source whose source parameters are known from closely drilling information, and the inversion results are in accord with the true values.
► The DAS requires only the computation of the first order derivatives of magnetic anomaly.
► The DAS method is insensitive to noise.
► The DAS method can produce more stable results than similar methods.
Journal: Journal of Applied Geophysics - Volume 88, January 2013, Pages 101–104