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This algorithm (and all other magnetic methods) only computes the depth to the bottom of magnetization contrasts.
Magnetic methods of prospecting detect buried features by locating the magnetic disturbances they cause: these were introduced in 1957 58 and use such machines as the proton magnetometer, the proton gradiometer, and the fluxgate gradiometer.
Expected orientations are further supported by non-destructive magnetic methods.
In petroleum exploration the combination of gravity and magnetic methods for reconnaissance survey is well established.
Gravity and magnetic methods are the classical tools to identify such structures.
Therefore, the magnetic methods are used to delineate the structural and lithological configuration of the basement rocks.
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Magnetic method is the oldest geophysical exploration method used in prospecting.
A fast and accurate in situ magnetic method has been developed.
Thus, the magnetic method, in this case, could be of a more value than the gravity method.
In general, the geophysical magnetic method is mainly based on the measurements and analysis of small variations in the earth's magnetic field within any area.
According to the data of the magnetic method the fast increase of the second harmonic amplitude of the magnetic field happened in final stage of test.
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