Evaluasi Teknik-Teknik Pemisahan Anomali Gravitasi menggunakan Data Gravitasi Sintetis
Abstract
Separating regional and residual anomalies is essential for gravity data interpretation, yet comparative evaluations of separation techniques using noisy three-dimensional (3D) models remain limited. This study compares Butterworth, Moving Average, Upward Continuation, and second-order polynomial methods across three synthetic 3D scenarios: an isolated target, closely spaced sources, and an asymmetric fault contact, contaminated with 5% white Gaussian noise. Optimal parameters were determined through radial average power spectrum (RAPS) analysis. Performance was assessed using four weighted indicators: root mean square error (RMSE), Pearson correlation coefficient (CC), signal-to-noise ratio (SNR), and regional depth estimation accuracy (%Z). The results show that method performance depends on target geometry. For the isolated target, Moving Average and Butterworth achieved the highest scores of 13 points each. Upward Continuation performed best for closely spaced sources and the asymmetric fault contact, scoring 14 and 13 points, respectively. Accordingly, Moving Average and Butterworth are recommended for simple isolated targets, whereas Upward Continuation is better suited to closely spaced sources and fault boundaries with strong lateral gradients. These findings guide method selection based on target geometry, although further validation using field data is required.
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DOI: https://doi.org/10.37905/geojpg.v5i2.41729
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