INTERPRETATION OF GRAVITY AND MAGNETIC ANOMALIES PERTAINING TO VERTICAL CONTACTS OF BLOCKS OF ROCK.
AERONAUTICAL CHART AND INFORMATION CENTER ST LOUIS MO LINGUISTIC SECTION
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The degree of details is investigated with which the relative differentiation of blocks of rock can be determined relative to density and magnetization. A general solution of the problem is presented, which makes it possible to determine the change of excess density and magnetization of the depth function. The influence of certain factors upon the level of the indeterminate form of the solution is evaluated. Each method of exploring geophysics has a certain, most characteristic, physical model of the geological medium, important from the point of view of practical application. Both for gravitational and magnetic exploration, simplest and most efficient is the case of the vertical bedding of rocks, when the changes of physical parameters and anomalies agree especially distinctly. Author
- Geology, Geochemistry and Mineralogy
- Magnetic and Electric Field Detection and Detectors