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
On the nature and peculiarities of waves registered in the first arrivals during seismic exploration on the Baltic Shield
1974 S. A. Ankudinov
Depth of electrical exploration by methods of dipole inductive profiling and ungrounded loop
1974 V. H. Zakharov