AERONAUTICAL CHART AND INFORMATION CENTER ST LOUIS MO LINGUISTIC SECTION
In order to minimize the difficulty of estimating magnetic and gravitational anomalies widely distributed in the upper part of the earths crust, and to lessen difficulty of determining the parameters of the perturbing bodies, it has been accepted to compare the anomalies above stratified bodies to the anomalies above inclined layers a body limited by two inclined and one horizontal plane. This makes it possible to study the characteristics of the anomalies and find the necessary method for the determination of the parameters of the perturbing body. In this study it is suggested that the graphic method be used for determining all the parameters of the inclined layer. For this purpose, log-log graticules, compiled for a sufficiently wide change of dimensions of the body under discussion, is recommended. Author
Trans. of mono. Interpretatsiya Magnitnykh i Gravitatsionnykh Anomalii nad Plastoobraznymi Telami, Moscow, 1963 39p.