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).

𝑁	𝑀 (m)	Depth 𝑧(m)	Shape factor 𝑞	Amplitude coefficient 𝐴 (mGal)	Standard error 𝜇(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