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Vol 61 Iss. 2
Pages:
49-54
Download volume:
RUS
Article

Some peculiarities of geological interpretation of gravitational and magnetic fields of Precambrian formations

Authors:
V. Kh. Zakharov
Date submitted:
1970-08-19
Date accepted:
1970-10-15
Date published:
1971-07-09

Abstract

Precambrian platforms and shields, occupying the main part of the territory of the continents and storing in their bowels huge reserves of minerals, are not sufficiently studied geologically. Dissection and correlation of Precambrian strata by classical methods of paleontological, petrographic and structural-geological analysis are extremely difficult, as deeply metamorphosed and granitized rocks in many cases retain only relict textural and lithological features of the original geological formations. Geophysical methods, in particular, gravity and magnetic exploration, have great potential in studying the structure and reconstructing the history of development of Precambrian shields.

Область исследования:
(Archived) Without section
Funding:

None

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References

  1. Kalyaev GI. Tectonics of the Precambrian of the Ukrainian Iron Ore Province. Naukova Dumka, 1965.
  2. Krutikhovskaya Z. A., Galenzovskaya V. I. I., Podolyanko S. M. Reflection of deep folding in physical fields of the West Inguletskaya zone. Geophys. coll., v. 16, Naukova Dumka, 1966.
  3. Kuzhelov G K. Geologic structure of Precambrian of Middle Pobuzhye on geophysical data. Geol. journal of the AS of the Ukr. SSR, vol. XX, iss. 2, 1960.
  4. Gilyarova M. A. Stratigraphy and Structure of the Pechenga. PH LSU, 1967
  5. Strygin A.I. Granitization of rocks and ore formation in the Ukrainian Shield. In the collection: Geology and Prospects of Metalliferousness of Precambrian Belorussia and Adjacent Regions. Science and Technology, 1965.
  6. Kratz K. O. Geology of the Karelian Karelides. PH of the AS USSR, 1963.
  7. Logachev A. A. Magnetic Prospecting. Nedra, 1968.

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