Decomposition of ∆T and Za magnetic anomaly of a three-dimensional source into natural orthogonal components
Authors:
Abstract
The anomaly of the harmonic approximation of the ∆T magnitude of a three-dimensional source is generally formed by five components of the magnetic field...
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(Archived) Without section
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None
References
- Afanasyev N.L. Method of calculation of potential fields in space and its application in exploration geophysics. Moscow, Nedra, 1968.
- Bat Marcus. Spectral Analysis in Geophysics. M., Nedra, 1980.
- Glazunov V.V. Component method of interpretation of isometric magnetic anomalies. VINITI, 5467-83 dep. L., 1983.
- Duboshin G.N. Theory of attraction. M., Nedra, 1964.
- Logachev A.A., Zakharov V.P. Magnetic Prospecting. L., Nedra, 1973.
- Strakhov V.N., Lapina M.I. Direct and Inverse Problem of Gravimetry and Magnetometry for Arbitrary Homogeneous Polyhedrons. - In the book: Theory and Practice of Interpretation of Gravitational and Magnetic Fields in the USSR. Kiev, Naukova Dumka, 1983.
- Tafeev G.P., Sokolov K.P. Geological interpretation of magnetic anomalies. L., Nedra, 1981.
- Tafeev Y.P. About calculations of the ∆T magnetic field. - In the book: Geophysical Exploration of Ore Deposits. Moscow, Gosgeoltekhizdat, 1953.
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