Glauconite Deposits in Russia: Geological Position, Formation Conditions, and Development Perspective; Lithology and Mineral Resources; Vol. 57, iss. 3

Bibliographic Details
Parent link:Lithology and Mineral Resources
Vol. 57, iss. 3.— 2022.— [P. 234-247]
Corporate Author: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии
Other Authors: Belousov P. E. Petr Evgenjevich, Chupalenkov N. M. Nikita Mikhaylovich, Rudmin M. A. Maksim Andreevich, Krupskaya V. V. Viktoriya Valerjevna
Summary:Title screen
The article is devoted to analysis of the glauconite resource base in Russia. The geotectonic and lithological-paleogeographic positions of deposits and large glauconite occurrences, and their formation conditions are considered. Based on the structural position, age, and spatial localization of deposits and occurrences, glauconite provinces are identified and the most promising areas for expanding the glauconite resource base in the Russian Federation are identified. Information on reserves in deposits, the degree of their development, and production volumes is given. An overview of the main producer countries and glauconite production volumes in the world is presented. The geological structure and quality of raw materials in the Karinsk glauconite deposit are described. In tectonic terms, the glauconite deposits and occurrences in Russia are confined to the central parts of plates and platforms, foredeeps, and orogenic belts. The majority of glauconite deposits and occurrences are found in the Upper Cretaceous and Paleogene (Late Jurassic or Early Cretaceous in some cases) rocks. Predicted glauconite resources in the Russian Federation are more than 2.5 Gt. The most promising sites include the areas of western Siberia, as well as Moscow and Kirov districts in the European part of Russia.
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.1134/S002449022202002X
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=668719

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330 |a The article is devoted to analysis of the glauconite resource base in Russia. The geotectonic and lithological-paleogeographic positions of deposits and large glauconite occurrences, and their formation conditions are considered. Based on the structural position, age, and spatial localization of deposits and occurrences, glauconite provinces are identified and the most promising areas for expanding the glauconite resource base in the Russian Federation are identified. Information on reserves in deposits, the degree of their development, and production volumes is given. An overview of the main producer countries and glauconite production volumes in the world is presented. The geological structure and quality of raw materials in the Karinsk glauconite deposit are described. In tectonic terms, the glauconite deposits and occurrences in Russia are confined to the central parts of plates and platforms, foredeeps, and orogenic belts. The majority of glauconite deposits and occurrences are found in the Upper Cretaceous and Paleogene (Late Jurassic or Early Cretaceous in some cases) rocks. Predicted glauconite resources in the Russian Federation are more than 2.5 Gt. The most promising sites include the areas of western Siberia, as well as Moscow and Kirov districts in the European part of Russia. 
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610 1 |a труды учёных ТПУ 
610 1 |a glauconite 
610 1 |a natural sorbents 
610 1 |a industrial minerals 
610 1 |a mineral resource base 
610 1 |a potassium fertilizers 
610 1 |a glauconite provinces 
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701 1 |a Belousov  |b P. E.  |g Petr Evgenjevich 
701 1 |a Chupalenkov  |b N. M.  |g Nikita Mikhaylovich 
701 1 |a Rudmin  |b M. A.  |c geologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of Geological and Mineralogical Sciences  |f 1989-  |g Maksim Andreevich  |3 (RuTPU)RU\TPU\pers\33254  |9 16999 
701 1 |a Krupskaya  |b V. V.  |g Viktoriya Valerjevna 
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