Optimum network calculation method of measurement in conditions of the latent periodicity of geological fields

At application of geometrical autocorrelation method there can be difficulties in calculation of an optimum network of measurement for the multistructural geological fields due to low-frequency components that shade high-frequency components. For the decision of a problem two ways are offered: 1) subtraction of a linear trend, 2) differentiation of geological fields. The second way is more effective.