2023
DOI: 10.1016/j.coal.2023.104265
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Provenance of multi-stage volcanic ash recorded in the Late Carboniferous coal in the Jungar Coalfield, North China, and their contribution to the enrichment of critical metals in the coal

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Cited by 21 publications
(5 citation statements)
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“…This can be supported by the Nb and Zr peaks found in the EDS spectra of anatase from noncoal samples. 25 Previous studies, e.g., Jiu et al, 45 Zhang et al, 47 and Zhang et al, 48 further supported such association of Zr, Hf, Nb, and Ta in coal.…”
Section: Analysis Of Datanhao Coalmentioning
confidence: 80%
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“…This can be supported by the Nb and Zr peaks found in the EDS spectra of anatase from noncoal samples. 25 Previous studies, e.g., Jiu et al, 45 Zhang et al, 47 and Zhang et al, 48 further supported such association of Zr, Hf, Nb, and Ta in coal.…”
Section: Analysis Of Datanhao Coalmentioning
confidence: 80%
“…Niobium (Nb), Tantalum (Ta), and Thorium (Th). Niobium and Ta are almost geochemically inseparable, 13,47,48 and as Dai et al 23 suggested, thorium in the Adaohai coal mainly comes from detrital materials of the source region, which may be the same source as Nb and Ta. Therefore, it is not surprising that Th and Nb are adjacent in the skeleton (Figure 7).…”
Section: Thorium (Th) and Uranium (U)mentioning
confidence: 97%
“…The enrichment of Ga in the top and bottom plates of the coal seams indicates that the Ga-containing carriers in the clay minerals entered the coal seams through the surrounding rocks under the action of groundwater, showing the influence of catagenesis, which indicates that the catagenesis leaching action and the activity of groundwater are other factors contributing to the enrichment of Ga in the Heidaigou coal-Ga deposit [20]. Moreover, in the clayey conglomerate of the Heidaigou coal series, significant quantities of volcanic clasts and volcanic ash have been identified [67,[77][78][79]. Earlier research on the Taiyuan Formation revealed thin layers of volcanic tuff [80], indicating that these volcanic tuff layers and clasts might have originated from volcanic activities along the orogenic belt at the boundary of the North China and South Mongolia Plates.…”
Section: Enrichment Genesis Of Heidaigou Coal-ga Depositmentioning
confidence: 97%
“…Due to the stable structural conditions, it was conducive to the formation of bauxite, and the moyite clastic materials of the Yinshan ancient land provided direct provenance for the study area [14,19]. Bauxite residue within the weathering crust was a source of Li, and the input of volcanic ash produced by volcanic activities affects the enrichment characteristics of Li [55,[58][59][60][61]. During the formation of Haerwusu Li-rich coal, the chemically altered detrital material of moyite from the Yinshan ancient land was initially enriched in the weathering crust of the Upper Carboniferous Benxi Formation after long-term surface efflorescence, denudation, and transport.…”
Section: Occurrence State and Origin Of Enrichment Of LI In Coalmentioning
confidence: 99%