Rhythmicity of the Lower Aldan coal-bearing formation and its relation to coalpotential
Authors:
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
References
- 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)
- 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)
- Ivanov G. A. Coal-Bearing Formations. Nauka, 1967. (in Russian)
- 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)
- 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)
- Ritenberg M. I. Distribution of coal bed thicknesses in the coal-bearing strata. DAN, vol. 131, No. 3, 1960. (in Russian)
- 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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