Peculiarities of coals of the gelitolite class and the conditions of their formation
Authors:
Abstract
The degree of participation of gelitolites in the structure of coal seams increases from the Lower Carboniferous to the Neogene. Whereas in the seams of the Lower Carboniferous they form thin layers, in the Middle Carboniferous they acquire seam-forming significance, forming seams of small and medium thickness. ...
Область исследования:
(Archived) Without section
Funding:
None
References
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