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The coordinate transformation matrices should be defined directly by using the "geological angles" strike, dip and rake, like Clark et al. (1986, p. 182) did. By using their approach, however, the matrix for oblate ellipsoids must be modified. I will try to implement the equations presented by Clark et al. (1986) and modify the equations for oblate ellipsoids.
Clark, D., Saul, S., and Emerson, D.: Magnetic and gravity anomalies of a triaxial ellipsoid, Exploration Geophysics, 17, 189–200, 1986.
The text was updated successfully, but these errors were encountered:
The coordinate transformation matrices should be defined directly by using the "geological angles" strike, dip and rake, like Clark et al. (1986, p. 182) did. By using their approach, however, the matrix for oblate ellipsoids must be modified. I will try to implement the equations presented by Clark et al. (1986) and modify the equations for oblate ellipsoids.
The text was updated successfully, but these errors were encountered: