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- W4386171157 abstract "Abstract The paper considers sections of the Visean coal-bearing formation of the Kama coal basin on the territory of the western slope of the South Tara arch. The sections are composed of coals, mudstones, siltstones, and sandstones, which were formed under continental conditions at the beginning of the Visean. The rocks of the coal-bearing formation were formed within the coastal shallow-marine plain with a lacustrine-marsh type of sedimentation. The formation of coals occurred during the formation of isolated swampy lakes on the surface of the floodplain lowlands. The source of organic matter was tree-like and herbaceous vegetation that develops in waterlogged lake water bodies in a hot, wet humid climate. According to the degree of coalification, coals belong to brown coals, their composition is dominated by a black, structureless, amorphous mass of coalified plant matter (fusen). As impurities, there are large fragments of plant remains belonging to the groups of intertinites and macerals. The coals are enriched in mineral, ash components, represented by kaolinite and finely dispersed quartz grains. Ash content will not exceed 20%." @default.
- W4386171157 created "2023-08-26" @default.
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- W4386171157 date "2023-08-01" @default.
- W4386171157 modified "2023-10-18" @default.
- W4386171157 title "Structure of coal-bearing sections of swampy coastal-marine lowlands of the Kama coal basin in the territory of the Tatarstan" @default.
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- W4386171157 doi "https://doi.org/10.1088/1755-1315/1229/1/012042" @default.
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