Three‐dimensional (3-D) interactive modeling permits integrated processing and interpretation of gravity and magnetic data, yielding an improved geologic interpretation. 3-D model bodies are constructed from polyhedra of suitable geometry and physical parameters (density and susceptibility), input on an interactive graphics terminal that is tied to a host computer. The method is especially designed for concurrent processing and interpretation in an interactive mode. The effect on gravity of a homogeneous polyhedron is calculated by transforming a volume integral into a sum of line integrals. Magnetic effects can be modeled by using either Poisson’s theorem or a slight modification of the formulas derived for gravity modeling. The interactive modeling program allows the user to change the geometry as well as the density and/or susceptibility of the elementary polyhedra and to observe results quickly during the course of processing. This capability enables the interpreter to decide immediately if and where ...
[1]
Hiroshi Akima,et al.
A Method of Bivariate Interpolation and Smooth Surface Fitting for Irregularly Distributed Data Points
,
1978,
TOMS.
[2]
M. Landisman,et al.
Rapid gravity computations for two‐dimensional bodies with application to the Mendocino submarine fracture zone
,
1959
.
[3]
D. Nagy.
The prism method for terrain corrections using digital computers
,
1966
.
[4]
F. S. Grant,et al.
REVIEW OF DATA PROCESSING AND INTERPRETATION METHODS IN GRAVITY AND MAGNETICS, 1964–71
,
1972
.
[5]
Manik Talwani,et al.
Rapid computation of gravitational attraction of three-dimensional bodies of arbitrary shape
,
1960
.
[6]
Lindrith Cordell,et al.
Iterative three-dimensional solution of gravity anomaly data using a digital computer
,
1968
.