Figure - available from: Frontiers in Earth Science
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DC results for different methods: (A) gravity anomaly at 500 m; (B) true value of the gravity anomaly at 0 m; (C) DC gravity anomaly at 0 m using the TEDC method; (D) DC gravity anomaly at 0 m using the DFDC method with a filter equal to 1000; (E) DC gravity anomaly at 0 m using the DC-Net model; (F) error between (B) and (E).
Source publication
Downward continuation (DC) of the gravity potential field is an important approach used to understand and interpret the density structure and boundary of anomalous bodies. It is widely used to delineate and highlight local and shallow anomalous sources. However, it is well known that direct DC transformation in the frequency domain is unstable and...
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