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"
Solved II. Following is the field gravity anomaly due to a
Application of the normalized largest eigenvalue of structure
Cross-gradient Joint Inversion of Gravity and Magnetic Anomaly
Remote Sensing, Free Full-Text
PDF) Normalized Full Gradient of Gravity Anomaly Method and Its
3D density imaging using gravity and gravity gradient in the
Minerals, Free Full-Text
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
3D density imaging using gravity and gravity gradient in the
New Semi-Inversion Method of Bouguer Gravity Anomalies Separation
Forward Modeling Research of Gravity Data Offset in North China Region
Efficient setup of initial model for solving 2D gravity anomaly
Gravity gradients