Fig. 3: a) gravity anomaly of a buried sphere at z=2 km, ρ=0.1 g/cm3, R=0.5 km, L=20 km, dx=0.5 km, b) Normalized full gradient of gravity anomaly due to the sphere. c) gravity anomaly of a buried vertical cylinder at depth to top is 1 km, ρ=0.1 g/cm3, R=0.5 km, L=10 km, dx=0.5 km, d) Normalized full gradient of gravity anomaly due to the vertical cylinder - "Normalized Full Gradient of Gravity Anomaly Method and Its Application to the Mobrun Sulfide Body, Canada"
Bouguer gravity anomaly of the profile, its corresponding GPS
Processing and interpretation of full tensor gravity anomalies of
Cross-gradient Joint Inversion of Gravity and Magnetic Anomaly
Application of the normalized largest eigenvalue of structure
Estimation of Depth to Salt Domes from Normalized Full Gradient of
Efficient setup of initial model for solving 2D gravity anomaly
The image of the normalized full gradient of the gravity profile
New Semi-Inversion Method of Bouguer Gravity Anomalies Separation
Adopting normalized full gradient method for regional‐scale
Gravity anomaly - Wikipedia
Solved II. Following is the field gravity anomaly due to a