First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam
This paper represents the first integrated research on the mineralogical, geochemical and stable isotope characteristics of the Upper Triassic high‑sulfur coals from the Khanh Hoa open-pit mine, Thai Nguyen Coalfield, NE Vietnam. Formed in a marine-influenced carbonate succession, the Khanh Hoa coal...
| Autores: | , , , , , , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2022 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/280833 |
| Acceso en línea: | http://hdl.handle.net/10261/280833 https://api.elsevier.com/content/abstract/scopus_id/85137630659 |
| Access Level: | acceso abierto |
| Palabra clave: | Upper Triassic Carbon and nitrogen isotopes High‑sulfur coals Hydrothermal activity Mo-U-Cs-Sb enrichment Thai Nguyen Coalfield |
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First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE VietnamLi, JingWang, YuanNguyen, XuanphuZhuang, XinguoLi, JianchengQuerol, XavierLi, BaoqingMoreno, NataliaHoang, VanlongCórdoba, PatriciaDo, VanthuatUpper TriassicCarbon and nitrogen isotopesHigh‑sulfur coalsHydrothermal activityMo-U-Cs-Sb enrichmentThai Nguyen CoalfieldThis paper represents the first integrated research on the mineralogical, geochemical and stable isotope characteristics of the Upper Triassic high‑sulfur coals from the Khanh Hoa open-pit mine, Thai Nguyen Coalfield, NE Vietnam. Formed in a marine-influenced carbonate succession, the Khanh Hoa coal is characterized by medium ash yield, low volatile matter yield, and high sulfur content. Minerals in the Khanh Hoa coal are predominantly composed of authigenic calcite in the upper portion; and pyrite, quartz, with minor amounts of tobelite ([(NH4), K] (Si, Al)4Al2O10(OH)2), gypsum in the middle and lower portions. The high‑sulfur Khanh Hoa coal is enriched in an As-Mo-Sb-U-Cs-P assemblage, which presents both an organic and inorganic mode of occurrence, and is largely ascribed to hydrothermal fluids. The δ13C values of the Khanh Hoa coal range from −24.77‰ to −22.80‰ (avg. −23.33‰), reflecting a change in sedimentation pattern (from transgressive to high stand system upwards). The δ15N values of the Khanh Hoa coal range from 2.41‰ to 3.73‰ (avg. 3.30‰), possibly resulted from influenced by seawater influence and a redox environment. The mineralogical, geochemical and isotopic characteristics reflected that the high‑sulfur Khanh Hoa coal was formed/preserved in marine-influenced anoxic environment, with low detrital input, and strong activities of multi-stage hydrothermal solutions.This research was supported by the National Key Research and Development Program of China (No. 2021YFC2902000), the National Natural Science Foundation of China (Nos. 41972179, 41972180), the Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) (No. CUGCJ1819), and the Key Project of Coal-based Low-carbon Joint Research Foundation of NSFC and Shanxi Province (No. U1910204). The authors express great gratitude to the editor and anonymous reviewers for their comments, which greatly improved the manuscript quality.Peer reviewedElsevierConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202220222022info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/280833https://api.elsevier.com/content/abstract/scopus_id/85137630659reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)InglésInternational Journal of Coal Geologyhttps://doi.org/10.1016/j.coal.2022.104097Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/2808332026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam |
| title |
First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam |
| spellingShingle |
First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam Li, Jing Upper Triassic Carbon and nitrogen isotopes High‑sulfur coals Hydrothermal activity Mo-U-Cs-Sb enrichment Thai Nguyen Coalfield |
| title_short |
First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam |
| title_full |
First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam |
| title_fullStr |
First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam |
| title_full_unstemmed |
First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam |
| title_sort |
First insights into mineralogy, geochemistry, and isotopic signatures of the Upper Triassic high‑sulfur coals from the Thai Nguyen Coal field, NE Vietnam |
| dc.creator.none.fl_str_mv |
Li, Jing Wang, Yuan Nguyen, Xuanphu Zhuang, Xinguo Li, Jiancheng Querol, Xavier Li, Baoqing Moreno, Natalia Hoang, Vanlong Córdoba, Patricia Do, Vanthuat |
| author |
Li, Jing |
| author_facet |
Li, Jing Wang, Yuan Nguyen, Xuanphu Zhuang, Xinguo Li, Jiancheng Querol, Xavier Li, Baoqing Moreno, Natalia Hoang, Vanlong Córdoba, Patricia Do, Vanthuat |
| author_role |
author |
| author2 |
Wang, Yuan Nguyen, Xuanphu Zhuang, Xinguo Li, Jiancheng Querol, Xavier Li, Baoqing Moreno, Natalia Hoang, Vanlong Córdoba, Patricia Do, Vanthuat |
| author2_role |
author author author author author author author author author author |
| dc.contributor.none.fl_str_mv |
Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Upper Triassic Carbon and nitrogen isotopes High‑sulfur coals Hydrothermal activity Mo-U-Cs-Sb enrichment Thai Nguyen Coalfield |
| topic |
Upper Triassic Carbon and nitrogen isotopes High‑sulfur coals Hydrothermal activity Mo-U-Cs-Sb enrichment Thai Nguyen Coalfield |
| description |
This paper represents the first integrated research on the mineralogical, geochemical and stable isotope characteristics of the Upper Triassic high‑sulfur coals from the Khanh Hoa open-pit mine, Thai Nguyen Coalfield, NE Vietnam. Formed in a marine-influenced carbonate succession, the Khanh Hoa coal is characterized by medium ash yield, low volatile matter yield, and high sulfur content. Minerals in the Khanh Hoa coal are predominantly composed of authigenic calcite in the upper portion; and pyrite, quartz, with minor amounts of tobelite ([(NH4), K] (Si, Al)4Al2O10(OH)2), gypsum in the middle and lower portions. The high‑sulfur Khanh Hoa coal is enriched in an As-Mo-Sb-U-Cs-P assemblage, which presents both an organic and inorganic mode of occurrence, and is largely ascribed to hydrothermal fluids. The δ13C values of the Khanh Hoa coal range from −24.77‰ to −22.80‰ (avg. −23.33‰), reflecting a change in sedimentation pattern (from transgressive to high stand system upwards). The δ15N values of the Khanh Hoa coal range from 2.41‰ to 3.73‰ (avg. 3.30‰), possibly resulted from influenced by seawater influence and a redox environment. The mineralogical, geochemical and isotopic characteristics reflected that the high‑sulfur Khanh Hoa coal was formed/preserved in marine-influenced anoxic environment, with low detrital input, and strong activities of multi-stage hydrothermal solutions. |
| publishDate |
2022 |
| dc.date.none.fl_str_mv |
2022 2022 2022 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Postprint info:eu-repo/semantics/acceptedVersion |
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article |
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acceptedVersion |
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http://hdl.handle.net/10261/280833 https://api.elsevier.com/content/abstract/scopus_id/85137630659 |
| url |
http://hdl.handle.net/10261/280833 https://api.elsevier.com/content/abstract/scopus_id/85137630659 |
| dc.language.none.fl_str_mv |
Inglés |
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Inglés |
| dc.relation.none.fl_str_mv |
International Journal of Coal Geology https://doi.org/10.1016/j.coal.2022.104097 Sí |
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info:eu-repo/semantics/openAccess |
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openAccess |
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Elsevier |
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Elsevier |
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reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
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Consejo Superior de Investigaciones Científicas (CSIC) |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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