About distribution of germanium in coal seams of paralic type deposits
Authors:
Abstract
The regularities of germanium distribution and causal relations of mineralization with the peculiarities of peat bog formation are shown on the example of a stratum of complex structure. The latter is represented by one complex coal seam or split into two, and the distance between them gradually increases from 10-15 cm to 10-12 meters. The areas with low thickness of the interbed are composed mainly of mudstones and less frequently siltstones. In areas with increasing interbed thickness, sandy-silty sediments appear ...
Область исследования:
(Archived) Without section
Funding:
None
Similar articles
Fractures and their relation to folding (on the example of the Atasuysky area in central Kazakhstan)
1965 B. G. Korenkov
On the structure of vein quartz of the Khrustalenosnoe deposit of the Ural Mountains
1965 V. Yu. Eshkin
About some peculiarities of the process of rebirth of granites into pegmatites in pegmatite veins of the Mamsky district
1965 V. N. Morakhovsky