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.
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