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Vol 60 Iss. 2
Pages:
112-118
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RUS
Article

Rhythmicity of the Lower Aldan coal-bearing formation and its relation to coal-bearing capacity

Authors:
G. P. Dubar
Date submitted:
1970-08-01
Date accepted:
1970-10-18
Date published:
1971-02-01

Abstract

The Nizhne-Aldansky District is located in the southeastern part of the Lena basin, east of the Tumara and Lena rivers.

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References

  1. Dubar G. P. et al. History of the Upper Mesozoic coal accumulation in the southeastern part of the Lena Basin. Proc. LAGU, USSR Academy of Sciences, vol. XVIII, 1963.
  2. Ivanov G. A. Methodology of facies-geotectonic analysis of coal-bearing deposits and its application in the practice of geological exploration. Proc. USSR, vol. V, 1956.
  3. Ivanov G. A. Coal-Bearing Formations. Nauka, 1967.
  4. Ivanov N. V. Structure and conditions of formation of the Chechum series of the southeastern part of the Lena Basin. Author's abstract of сand. dissertation, LMI, 1962.
  5. Makedonov A. V. Paragenesis of coals, host rocks and nodules of the Vorkutokoi Formation and methods of coal-bearing capacity prediction. Proc. LAGU, USSR Academy of Sciences, iss. V, 1956.
  6. Ritenberg M. I. Distribution of coal beds thicknesses in the coal-bearing strata. RAS, vol. 131, No. 3, 1960.
  7. Salnikov B. A. Coal-bearing cycles of sedimentation of the Upper Duy Formation of the West Coast of Sakhalin. In the collection: Problems of Geology of Coal-bearing Sediments of the Asian Part of the USSR. PH AS USSR, 1961.

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