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

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

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.

Область исследования:
(Archived) Without section
Funding:

None

Go to volume 60

References

  1. Dubar G. P. et al. History of the Upper Mesozoic coal accumulation in the southeastern part of the Lena Basin. Tr. LAGU AN SSSR, iss. XVIII, 1963. (in Russian)
  2. Ivanov G. A. Methodology of facies-geotectonic analysis of coal-bearing deposits and its application in the practice of geological exploration. Tr. LAGU AN SSSR, iss. V, 1956. (in Russian)
  3. Ivanov G. A. Coal-Bearing Formations. Nauka, 1967. (in Russian)
  4. Ivanov N. V. Structure and conditions of formation of the Chechum series of the southeastern part of the Lena Basin. Avtoref. kand. diss., LGI, 1962. (in Russian)
  5. Makedonov A. V. Paragenesis of coals, host rocks and nodules of the Vorkuta Formation and methods of coal-bearing capacity prediction. Tr. LAGU AN SSSR, iss. V, 1956. (in Russian)
  6. Ritenberg M. I. Distribution of coal bed thicknesses in the coal-bearing strata. DAN, vol. 131, No. 3, 1960. (in Russian)
  7. Salnikov B. A. Coal-bearing cycles of sedimentation of the Upper Duy Formation of the West Coast of Sakhalin. Sb. "Voprosy geologii uglenosnykh otlozhenii Aziatskoi chasti SSSR". Izd-vo AN SSSR, 1961. (in Russian)

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