Determination of magnetization direction and geometrical parameters of depth-limited formations by magnetic field
Abstract
During magnetic surveys, anomalies are often detected, the nature of which rather clearly reflects the influence of the lower boundary of magnetized bodies of bedded form. The use of the anomalous magnetic field to estimate the possible down-dip extent of such bodies and to determine the dip angle may be of important significance in prospecting and exploration of many ore deposits and in solving various structural problems.
Область исследования:
(Archived) Without section
Funding:
None
References
- Bulina L. V. On the use of aeromagnetic survey materials in the study of the deep structure of the Earth's crust. Sovetskaya geologiya , 1961, No. 5 (in Russian)
- Zakharov V. P. Use of magnetic survey data in determining the dip angles of arbitrarily magnetized bedded bodies. Zapiski Gornogo Instituta, 1971, vol. 61, issue 2 (in Russian)
- Ivanov S. S. On the determination of the depths of occurrence of the lower boundary of magnetic bodies. Vestn. Mosk. un-ta, Geologiya y, 1968, No. 5 (in Russian)
- Logachev A. A. Magnetic Prospecting. M., Nedra, 1968 (in Russian)
- Shalaev S. V. Application of functions of a complex variable in the geological interpretation of gravity and magnetic data. Vopr. razvedochnoi geofiziki , 1960, issue 1 (in Russian)
- Shimaraev V. N. On the calculation of the lower edge of a vertically magnetized bed. In the book: Geophys. Methods of Exploration in the Arctic, issue 5, L., Izd. NIIGA, 1968 (in Russian)
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