Submit an Article
Become a reviewer
Vol 49 Iss. 2
Pages:
60-68
Download volume:
RUS
Article

Acidic Lower Cretaceous subvolcanic and volcanic formations of the North Argun Depression

Authors:
P. A. Strona
N. F. Kiseleva
Date submitted:
1964-08-17
Date accepted:
1964-10-08
Date published:
1965-12-03

Abstract

In the complex history of Mesozoic magmatism and ore formation in Eastern Transbaikalia, the latest stages of the history, associated with the formation of numerous linearly elongated depressions of northeastern strike, are the least studied. They are bordered by large faults and are filled with Late Mesozoic sedimentary and volcanogenic rocks. It is to the depressions that the areas of the strongest manifestation of young tectonic movements and occurrence of the latest magmatic formations gravitate. Accordingly, the latest manifestations of hydrothermal mineralization in Eastern Transbaikalia are closely related to the depressions themselves or to the systems of faults surrounding them (gold deposits of the Baley type, deposits of fluorspar, ferberite‑antimonite ores of the Barun‑Shivey type, ore occurrences of antimonite, cinnabar, barite, etc.). The overwhelming majority, if not all these ore occurrences, belong to the type of low‑temperature hydrothermal formations of shallow depths. Both the source of this mineralization and its age are still controversial. However, in recent years the opinion has been expressed that this mineralization is related to the Lower Cretaceous volcanogenic complexes. Therefore, it is very important to study the history of Lower Cretaceous volcanism of Eastern Transbaikalia, in particular, to investigate various subvolcanic, vent, etc. formations, since in a number of geologically similar areas their location largely determines the distribution of mineralization ...

Область исследования:
(Archived) Without section
Funding:

None

Go to volume 49

References

  1. Vinogradov A. P. Regularities of distribution of chemical elements in the Earth's crust. Geokhimiya, No. 1 and 6, 1956.
  2. Sobolev V. S. Significance of ferruginousness of femic minerals. Mineralogicheskiy sbornik L'vovskogo geologicheskogo obshchestva, No. 4, 1950.
  3. Strona P. A. To the question about the sources of low-temperature hydrothermal mineralization in the Eastern Transbaikalia. Geologiya rudnykh mestorozhdeniy, No. 4, 1962.
  4. Fogelman N. A. Some features of geology and metallogeny of the Baleisko-Darasun gold-bearing district (Eastern Transbaikalia). Trudy TsNIGRI, vol. 41 1962.

Similar articles

Middle-Upper Proterozoic formations of the Keivsky area of the Kola Peninsula
1965 V. A. Shkvorov
On the structure of vein quartz of the crystal‑bearing deposit of the Urals
1965 V. Yu. Eshkin
On the conditions of formation of the oxidation zone of the Osenneye molybdenum deposit
1965 S. V. Sendek
About some peculiarities of the process of rebirth of granites into pegmatites in pegmatite veins of the Mamsky district
1965 V. N. Morakhovsky
Reply to the remarks of B. Ya. Yufa on the article “ On the methodology of accounting for systematic error in determining the most reliable content of components in ores”.
1965 G. S. Porotov
Some features of Late Upper Jurassic effusives of Priargunya and their metallogenic significance
1965 P. A. Strona, N. F. Kiseleva