Determination of magnetization direction and geometrical parameters of depth-limited formations by magnetic field
Abstract
When conducting magnetic surveys, anomalies are often revealed, the nature of which quite clearly reflects the influence of the lower boundary of magnetized bodies of formation form. The use of anomalous magnetic roll to estimate the possible dip distribution of such bodies and to determine the dip angle may be important in prospecting and exploration of many ore deposits, solving various structural problems.
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(Archived) Without section
References
- Bulina L. V. On the use of aeromagnetic survey materials in the study of the deep structure of the Earth's crust. - Sov. Geology, 1961, No. 5.
- Zakharov V. P. Use of Magnetic Survey Data in Determining the Angles of Dip of Arbitrarily Magnetized Formation Bodies. - Journal of Mining Institute, 1971, vol. 61, iss. 2.
- Ivanov S. S. On Determination of Depths of Occurrence of the Lower Boundary of Magnetic Bodies. Journal of Moscow State University, Geology. 1968, № 5.
- Logachev A. A. Magnetic Prospecting. M., Nedra, 1968.
- Shalaev S. V. Application of Complex Variable Functions in Geological Interpretation of Gravity and Magnetic Data. - Issues of Exploration Geophysics, 1960, iss. 1.
- Shimaraev V. N. About calculation of the lower edge of the vertical magnetized layer. In the book: Geophys. Methods of Exploration in the Arctic, vol. 5, L., NIIGA, 1968.
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