Mineralogy and Geochemistry of the Lower Cretaceous Coals in the Junde Mine, Hegang Coalfield, Northeastern China
Hegang coalfield is one of the areas with abundant coal resources in Heilongjiang Province. Characteristics of minerals and geochemistry of No. 26 coal (lower Cretaceous coals) from Junde mine, Hegang coalfield, Heilongjiang province, China, were reported. The results showed that No. 26 coal of Jund...
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2022-07-01
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| Online Access: | https://www.mdpi.com/1996-1073/15/14/5078 |
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| author | Yingchun Wei Wenbo He Guohong Qin Anmin Wang Daiyong Cao |
| author_facet | Yingchun Wei Wenbo He Guohong Qin Anmin Wang Daiyong Cao |
| author_sort | Yingchun Wei |
| collection | DOAJ |
| description | Hegang coalfield is one of the areas with abundant coal resources in Heilongjiang Province. Characteristics of minerals and geochemistry of No. 26 coal (lower Cretaceous coals) from Junde mine, Hegang coalfield, Heilongjiang province, China, were reported. The results showed that No. 26 coal of Junde mine is slightly enriched in Cs, Pb, and Zr compared with world coals. The minerals in No. 26 coal of Junde mine primarily include clay minerals and quartz, followed by calcite, siderite, pyrite, monazite, and zircon. The diagrams of Al<sub>2</sub>O<sub>3</sub>–TiO<sub>2</sub>, Zr/Sc–Th/Sc, Al<sub>2</sub>O<sub>3</sub>/TiO<sub>2</sub>–Sr/Y, and Al<sub>2</sub>O<sub>3</sub>/TiO<sub>2</sub>–La/Yb indicate that the enriched elements in No. 26 coal were mainly sourced from the Late Paleozoic meta-igneous rocks in Jiamusi block. The volcanic ash contribution to No. 26 coal seems very low. Sulfate sulfur indicating oxidation/evaporation gradually decreases during No. 26 coal formation. |
| first_indexed | 2024-03-09T10:19:18Z |
| format | Article |
| id | doaj.art-7967bc36aa8f4e77b9add1165fb29ce5 |
| institution | Directory Open Access Journal |
| issn | 1996-1073 |
| language | English |
| last_indexed | 2024-03-09T10:19:18Z |
| publishDate | 2022-07-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Energies |
| spelling | doaj.art-7967bc36aa8f4e77b9add1165fb29ce52023-12-01T22:06:25ZengMDPI AGEnergies1996-10732022-07-011514507810.3390/en15145078Mineralogy and Geochemistry of the Lower Cretaceous Coals in the Junde Mine, Hegang Coalfield, Northeastern ChinaYingchun Wei0Wenbo He1Guohong Qin2Anmin Wang3Daiyong Cao4State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Beijing 100083, ChinaCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, ChinaSchool of Geographic Sciences/Hebei Key Laboratory of Environmental Change and Ecological Construction, Hebei Normal University, Shijiazhuang 050024, ChinaCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, ChinaState Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Beijing 100083, ChinaHegang coalfield is one of the areas with abundant coal resources in Heilongjiang Province. Characteristics of minerals and geochemistry of No. 26 coal (lower Cretaceous coals) from Junde mine, Hegang coalfield, Heilongjiang province, China, were reported. The results showed that No. 26 coal of Junde mine is slightly enriched in Cs, Pb, and Zr compared with world coals. The minerals in No. 26 coal of Junde mine primarily include clay minerals and quartz, followed by calcite, siderite, pyrite, monazite, and zircon. The diagrams of Al<sub>2</sub>O<sub>3</sub>–TiO<sub>2</sub>, Zr/Sc–Th/Sc, Al<sub>2</sub>O<sub>3</sub>/TiO<sub>2</sub>–Sr/Y, and Al<sub>2</sub>O<sub>3</sub>/TiO<sub>2</sub>–La/Yb indicate that the enriched elements in No. 26 coal were mainly sourced from the Late Paleozoic meta-igneous rocks in Jiamusi block. The volcanic ash contribution to No. 26 coal seems very low. Sulfate sulfur indicating oxidation/evaporation gradually decreases during No. 26 coal formation.https://www.mdpi.com/1996-1073/15/14/5078trace elementsmineralssourcevolcanicsedimentary environment |
| spellingShingle | Yingchun Wei Wenbo He Guohong Qin Anmin Wang Daiyong Cao Mineralogy and Geochemistry of the Lower Cretaceous Coals in the Junde Mine, Hegang Coalfield, Northeastern China Energies trace elements minerals source volcanic sedimentary environment |
| title | Mineralogy and Geochemistry of the Lower Cretaceous Coals in the Junde Mine, Hegang Coalfield, Northeastern China |
| title_full | Mineralogy and Geochemistry of the Lower Cretaceous Coals in the Junde Mine, Hegang Coalfield, Northeastern China |
| title_fullStr | Mineralogy and Geochemistry of the Lower Cretaceous Coals in the Junde Mine, Hegang Coalfield, Northeastern China |
| title_full_unstemmed | Mineralogy and Geochemistry of the Lower Cretaceous Coals in the Junde Mine, Hegang Coalfield, Northeastern China |
| title_short | Mineralogy and Geochemistry of the Lower Cretaceous Coals in the Junde Mine, Hegang Coalfield, Northeastern China |
| title_sort | mineralogy and geochemistry of the lower cretaceous coals in the junde mine hegang coalfield northeastern china |
| topic | trace elements minerals source volcanic sedimentary environment |
| url | https://www.mdpi.com/1996-1073/15/14/5078 |
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