宁东煤田横城矿区山西组3号煤的矿物和地球化学特征及关键金属的富集机理
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1.中国地质大学(武汉);2.宁夏回族自治区煤炭地质局

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宁夏2023年自治区财政地质资源勘探专项项目(640000233000000011005);宁夏回族自治区非常规天然气勘查开发创新团队资助项目(2022BSB03105)


Mineralogical and geochemical characteristics and enrichment mecha-nisms of critical elements in the No. 3 coal seam of the Shanxi Formation in the Hengcheng mining area, Ningdong coalfield
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1.China University of Geosciences;2.Ningxia Hui Autonomous Region Bureau of Coal Geology;3.中国地质大学(武汉)

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    摘要:

    煤系关键金属矿床的研究已成为煤地质学的前沿热点问题,也是关键金属矿产增储的重要来源。本文以宁东煤田横城矿区马莲台煤矿早二叠世山西组3号煤为研究对象,对其矿物和地球化学组分开展系统研究,以便查明煤中关键金属的分布、赋存和富集特征,并对其综合利用进行了评价。结果表明:①马莲台3号煤以中等灰分产率、高挥发分产率、特低全水分含量和低—中等全硫含量为特征,煤中矿物主要由高岭石组成;②煤中常量元素主要由SiO2和Al2O3组成,含少量Fe2O3、CaO和MgO。对比于世界煤均值,研究煤中Li和Zr达到富集程度,Ga、Nb、Hf、Ta、Pb、Th和稀土元素(REE+Y)达到轻度富集;③Li和Ga主要赋存在高岭石中,Zr(Hf)和Nb(Ta)主要赋存于锆石,REY主要赋存于高岭石及与高岭石共生的铝磷酸盐矿物中(磷铝钡石)。宁东煤田东北部的阴山古陆为马莲台3号煤提供了重要的长英质碎屑物质,此外阿拉善地块也提供了一定的火山碎屑物质。煤中Li 、Zr(Hf)和Nb(Ta)等关键金属的富集主要受控于长英质的碱性-过碱性碎屑物质输入量,化学风化作用和水/岩作用是次要控制因素。Ga的富集受控于化学风化作用强度。REY的富集主要受控于碎屑物质输入和水/岩作用过程。此外,高岭石的含量也是影响Li、Ga和REY富集的因素。马莲台3号煤可作为Li-Ga-Zr-REY潜在金属来源。

    Abstract:

    The study of coal-related critical elements deposits has become a frontier hotspot in coal geology research and an important source for increasing reserves of critical elements mineral resources. This study focuses on the No. 3 coal seam of the Early Permian Shanxi Formation at the Maliantai Coal Mine in the Hengcheng mining area of the Ningdong coalfield. It investigates the mineral composition and geochemistry to determine the distribution, occurrence, and en-richment characteristics of elements minerals in the coal, as well as to evaluate their compre-hensive utilization. The study results show that:(1)The No. 3 coal seam at Maliantai is characterized by medium ash yield, high volatile yield, ultra-low total moisture content, and low to medium total sulfur content, with minerals in the coal mainly composed of kaolinite;(2)The major elements in the coal are primarily composed of SiO2 and Al2O3, with minor amounts of Fe2O3, CaO, and MgO. Compared to the average coal worldwide, Li and Zr reach enrichment levels, while Ga, Nb, Hf, Ta, Pb, Th, and rare earth elements (REE+Y) are slightly enriched;(3)Li and Ga are mainly found in kaolinite, Zr (Hf) and Nb (Ta) are primarily found in zircon, and REY is primarily hosted in kaolinite and aluminum phosphate (goyazite) associated with kao-linite. The Yinshan ancient land in the northeast of Ningdong coal field provides important felsic clastic material for the Malitai No. 3 coal, in addition, the Alashan block also provides some volcanic clastic material. The enrichment of critical metals such as Li, Zr (Hf), and Nb (Ta) in the coal is mainly controlled by the input of alkaline-peralkaline felsic clastic materials, with chemical weathering and water-rock interactions being secondary controlling factors. The en-richment of Ga is primarily controlled by the intensity of chemical weathering. The enrichment of REY is mainly influenced by the input of clastic materials and water-rock interaction processes. In addition, the kaolinite content also plays a role in the enrichment of Li, Ga, and REY. Malian Tai No. 3 coal has potential as a source of Li-Ga-Zr-REY metals.

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  • 收稿日期:2024-08-01
  • 最后修改日期:2024-10-25
  • 录用日期:2024-10-29
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