About complexing of detailed gravity survey with microseismic survey at geological mapping
Abstract
In geologic mapping of ore districts on a large scale (1:50,000, 1:25,000 and larger), detailed gravity survey is widely used, which makes it possible to reveal many features of the geologic structure of bedrock overlain by loose sediments.
Область исследования:
(Archived) Without section
References
- Brodovoy V. V., Tsaregradsky V. A. Role of high-precision gravimetry in the search for copper and polymetallic deposits in Kazakhstan. In the book: Geophys. Research in Kazakhstan. Alma-Ata, Kazakhstan, 1968.
- Bulakh E.G. Integral ratio for interpretation of gravity anomalies. Kiev, Naukova Dumka, 1965.
- Geophysical studies in geologic mapping. Alma-Ata, Kazakhstan, 1968.
- Klushin I. G. Complex application of geophysical methods for solving geologic problems. L., Nedra, 1968.
- Logachev A. A. Magnetic Prospecting, L., Nedra, 1968.
- Muzylev V. S. Questions of Exploration Geophysics. Seismic Exploration. L., Nedra, 1966.
- Enenstein B. S. Non-parametric method of determining the depth of the crystalline basement roof by frequency sounding curves. - FEAS USSR, 1968, vol. 181, No. 2.
- Gгапt F. S., West G. F. Interpretation Theory in Applied geophysics. N. Y. Mc-Graw Hill В. C. 1964.
Similar articles
About macro- and microrelief of the Mohorovičić discontinuity on the Baltic Shield
1974 I. V. Litvinenko, L. N. Platonenkova, N. I. Suvorova
Geophysical data on the structure of the southeastern part of the Wind Belt synclinorium
1974 N. N. Bolgurtsev
Determination of magnetization direction and geometrical parameters of depth-limited formations by magnetic field
1974 V. P. Zakharov, S. G. Alekseev