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Vol 51 Iss. 2
Pages:
111-113
Download volume:
RUS
Article

Isotopic composition of argon and xenon from methane gases of the Khibiny massif

Authors:
I. N. Tolstikhin
Yu. A. Shukolyukov
G. I. Voitov
Date submitted:
1965-08-29
Date accepted:
1965-10-14
Date published:
1966-07-26

Abstract

The question of the origin of hydrocarbon gases of the Khibiny and Lovo-Zersky alkaline intrusive massifs has not been finally solved so far.According to I. A. Petersilie. There are three hypotheses about the origin of hydrocarbon gases: 1) due to assimilation and processing of organic compounds of the Imandra-Varzuga Formation by the magmatic melt; 2) in the magmatic melt (in the form of gas flow they rise to the surface parts of the lithosphere); 3) in the process of intrusion formation, simultaneously with the formation of magmatic rocks ...

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References

  1. Vinogradov, A. P. Average content of chemical elements in the main types of erupted rocks of the Earth's crust. Geochemistry, No. 7, 1962.
  2. Gerling E. K., Shchukolyukov Y. A. Application of spontaneous fission for the purposes of geochronology. Intern. geol. congr., XXII session, Reports of the Soviet Geol. PH of the AS USSR, 1964.
  3. Ivanov T. N. Apatite deposits of the Khibiny tundras. Gosgeoltekhizdat, 1963.
  4. Petersilie I. A. Geology and geochemistry of natural gases and dispersed bitumens of some geologic formations of the Kola Peninsula. Nauka, 1964.
  5. Shukolyukov Y. A., Tolstikhin I. N. Helium, argon and xenon in natural gases, Geochemistry, No. 7, 1965.
  6. Wasserburg G. J., E. Mazog. R. Е. Zartman. Isotopic and chemical composition of some terrestmal natural gases, Earth Science and Meteoritics, Amsterdam, 1963.
  7. Zartman R. E., Wasserburg G. J., Raynolds J. H. J. Geo- phys. Res., v. 66, No. 1, 1961.

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