Nodules in carbonaceous sediments of the Southern Tunguska basin |
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Authors: | N I Akulov |
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Institution: | (1) Institute of the Earth’s Crust, Siberian Division of the Russian Academy of Sciences, ul. Lermontova 128, Irkutsk, 664033, Russia |
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Abstract: | Pioneer results of the comprehensive analysis of nodules from the Upper Paleozoic coaliferous association and the underlying
Middle Paleozoic sequence in the southern Tunguska Basin (Siberian Craton) suggest the following: (1) sediments underlying
the coaliferous association contain two (siliceous and carbonate) types of normal nodules and one type of allogenic nodules
(redeposited chalcedony nodules in the kaolin-itechalcedony unit of the Beloyarsk Formation); (2) the coaliferous association
includes four (calcite, siderite, pyrite, and goethite) types of nodules; (3) each nodule type is confined to a specific genetic
type of sediment; e.g., siliceous nodules are confined to lagoonal sediments; calcite nodules, to lacustrine and lacustrine-boggy
sediments; siderite nodules, to lacustrine-boggy and boggy sediments; pyrite nodules, to boggy sediments; and goethite nodules,
to alluvial sediments; (4) the formation of goethite nodules is mainly related to the erosion and redeposition of siderite
nodules; (5) the coefficient of carbon concentration shows a distinct positive correction with the coefficient of nodule content;
(6) nodules appeared in the coaliferous association during diagenesis and epigenesis; the calcite and pyrite nodules are enriched
in sandy material, as suggested by the high content of insoluble residue; (7) combustion of coal seams promoted the melting
of the adjacent siderite nodules and the formation of magnetite ores; consequently, the thermally altered mudstones, siltstones,
and sandstones were transformed into a high-quality building material that is used as road fill. |
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