Research Article
A Fast Interpretation Method for Inverse Modeling of Residual Gravity Anomalies Caused by Simple Geometry
Table 6
Numerical results of the present method applied to the Mobrun field example, Canada (best-fit in bold).
| | (m) | Depth (m) | Shape factor | Amplitude coefficient (mGal) | Standard error (mGal) |
| 33.50 | 67.00 | 25.68 | 0.61 | 55.75 | 0.49 | 33.50 | 100.50 | 26.54 | 0.64 | 55.48 | 0.34 | 33.50 | 134.00 | 28.66 | 0.71 | 55.51 | 0.13 | 67.00 | 100.50 | 28.64 | 0.68 | 56.07 | 0.16 | 67.00 | 134.00 | 33.34 | 0.78 | 59.10 | 0.02 | 100.50 | 134.00 | 42.36 | 0.93 | 72.38 | 0.21 | −33.50 | −67.00 | 24.89 | 0.52 | 58.71 | 1.01 | −33.50 | −100.50 | 29.53 | 0.64 | 57.14 | 0.16 | −33.50 | −134.00 | 30.74 | 0.68 | 57.45 | 0.08 | −67.00 | −100.50 | 41.30 | 0.84 | 68.43 | 0.14 | −67.00 | −134.00 | 40.14 | 0.82 | 66.46 | 0.11 | −100.50 | −134.00 | 38.15 | 0.79 | 63.86 | 0.06 |
| Average (m) | | 32.50 | 0.72 | 60.53 | 0.06 |
|
|