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Geological Characteristics and Control Mechanism of Uranium Enrichment in Coal-Bearing Strata in the Yili Basin, Northwest China—Implications for Resource Development and Environmental Protection
[Image: see text] Uranium enrichment is considerably prevalent in Jurassic coal-bearing strata in the Yili Basin. A large amount of uranium deposits (occurrences) have been discovered in recent decades. Previous studies have found that uranium deposits and coal seam have a certain correlation in the...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Chemical Society
2022
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8851618/ https://www.ncbi.nlm.nih.gov/pubmed/35187361 http://dx.doi.org/10.1021/acsomega.1c06754 |
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author | Bai, Hongyang Wang, Wenfeng Lu, Qingfeng Wang, Wenlong Feng, Shuo Zhang, Bofei |
author_facet | Bai, Hongyang Wang, Wenfeng Lu, Qingfeng Wang, Wenlong Feng, Shuo Zhang, Bofei |
author_sort | Bai, Hongyang |
collection | PubMed |
description | [Image: see text] Uranium enrichment is considerably prevalent in Jurassic coal-bearing strata in the Yili Basin. A large amount of uranium deposits (occurrences) have been discovered in recent decades. Previous studies have found that uranium deposits and coal seam have a certain correlation in their genesis and spatial distribution or sometimes uranium deposits develop directly in the coal seam. What are the geological characteristics of uranium enrichment? How is uranium enriched? How to strengthen the cooperative development of uranium and coal and environmental protection? In order to explain the aforementioned questions, the characteristics of uranium deposits, rock minerals, and geochemical and metallogenic chronology are summarized herein, and the geological control mechanism of uranium enrichment in coal-bearing strata is discussed. It is found that uranium enrichment (including sandstone uranium deposits and coal uranium deposits) has multistage genetic characteristics and is mainly spread over the gentle slope of the southern margin of the Yili basin, with its host rock possibly being sandstone, coal, and sometimes even mudstone. The uranium concentration has a considerable correlation with the reductant, and the occurrence state of uranium has both inorganic and organic affinities. In addition, uranium enrichment is believed to be a comprehensive effect of high uranium source rocks, tectonic activity, sedimentary facies, hydrogeology conditions, paleoclimate, and reductant. The difference is that uranium enrichment in sandstone is often generated in a mud-sand-mud stratigraphic structure, while uranium enrichment in coal usually develops as coal-sand-mud. What is more, strengthening the study of physical and chemical properties of the host rock, strengthening the study of uranium occurrence state, and sharing geological data are important ways for the cooperative development of coal and uranium resources and environmental protection. |
format | Online Article Text |
id | pubmed-8851618 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | American Chemical Society |
record_format | MEDLINE/PubMed |
spelling | pubmed-88516182022-02-18 Geological Characteristics and Control Mechanism of Uranium Enrichment in Coal-Bearing Strata in the Yili Basin, Northwest China—Implications for Resource Development and Environmental Protection Bai, Hongyang Wang, Wenfeng Lu, Qingfeng Wang, Wenlong Feng, Shuo Zhang, Bofei ACS Omega [Image: see text] Uranium enrichment is considerably prevalent in Jurassic coal-bearing strata in the Yili Basin. A large amount of uranium deposits (occurrences) have been discovered in recent decades. Previous studies have found that uranium deposits and coal seam have a certain correlation in their genesis and spatial distribution or sometimes uranium deposits develop directly in the coal seam. What are the geological characteristics of uranium enrichment? How is uranium enriched? How to strengthen the cooperative development of uranium and coal and environmental protection? In order to explain the aforementioned questions, the characteristics of uranium deposits, rock minerals, and geochemical and metallogenic chronology are summarized herein, and the geological control mechanism of uranium enrichment in coal-bearing strata is discussed. It is found that uranium enrichment (including sandstone uranium deposits and coal uranium deposits) has multistage genetic characteristics and is mainly spread over the gentle slope of the southern margin of the Yili basin, with its host rock possibly being sandstone, coal, and sometimes even mudstone. The uranium concentration has a considerable correlation with the reductant, and the occurrence state of uranium has both inorganic and organic affinities. In addition, uranium enrichment is believed to be a comprehensive effect of high uranium source rocks, tectonic activity, sedimentary facies, hydrogeology conditions, paleoclimate, and reductant. The difference is that uranium enrichment in sandstone is often generated in a mud-sand-mud stratigraphic structure, while uranium enrichment in coal usually develops as coal-sand-mud. What is more, strengthening the study of physical and chemical properties of the host rock, strengthening the study of uranium occurrence state, and sharing geological data are important ways for the cooperative development of coal and uranium resources and environmental protection. American Chemical Society 2022-02-03 /pmc/articles/PMC8851618/ /pubmed/35187361 http://dx.doi.org/10.1021/acsomega.1c06754 Text en © 2022 The Authors. Published by American Chemical Society https://creativecommons.org/licenses/by-nc-nd/4.0/Permits non-commercial access and re-use, provided that author attribution and integrity are maintained; but does not permit creation of adaptations or other derivative works (https://creativecommons.org/licenses/by-nc-nd/4.0/). |
spellingShingle | Bai, Hongyang Wang, Wenfeng Lu, Qingfeng Wang, Wenlong Feng, Shuo Zhang, Bofei Geological Characteristics and Control Mechanism of Uranium Enrichment in Coal-Bearing Strata in the Yili Basin, Northwest China—Implications for Resource Development and Environmental Protection |
title | Geological Characteristics and Control Mechanism of
Uranium Enrichment in Coal-Bearing Strata in the Yili Basin, Northwest
China—Implications for Resource Development and Environmental
Protection |
title_full | Geological Characteristics and Control Mechanism of
Uranium Enrichment in Coal-Bearing Strata in the Yili Basin, Northwest
China—Implications for Resource Development and Environmental
Protection |
title_fullStr | Geological Characteristics and Control Mechanism of
Uranium Enrichment in Coal-Bearing Strata in the Yili Basin, Northwest
China—Implications for Resource Development and Environmental
Protection |
title_full_unstemmed | Geological Characteristics and Control Mechanism of
Uranium Enrichment in Coal-Bearing Strata in the Yili Basin, Northwest
China—Implications for Resource Development and Environmental
Protection |
title_short | Geological Characteristics and Control Mechanism of
Uranium Enrichment in Coal-Bearing Strata in the Yili Basin, Northwest
China—Implications for Resource Development and Environmental
Protection |
title_sort | geological characteristics and control mechanism of
uranium enrichment in coal-bearing strata in the yili basin, northwest
china—implications for resource development and environmental
protection |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8851618/ https://www.ncbi.nlm.nih.gov/pubmed/35187361 http://dx.doi.org/10.1021/acsomega.1c06754 |
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