首页|黔西北煤田晚二叠世煤关键金属Li-Nb-Ta富集特征及成因机制

黔西北煤田晚二叠世煤关键金属Li-Nb-Ta富集特征及成因机制

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关键金属是当今社会必须的但是安全供应存在高风险的一类金属的总称.煤因富含有机质往往能够富集关键金属,特殊地质条件下能形成煤型关键金属矿床.很多研究表明我国西南地区晚二叠世含煤地层富含多种关键金属,但是其富集特征和形成机制仍然不清楚.本文以贵州黔西北煤田泰来煤矿上二叠统龙潭组9#煤层为研究对象,系统采集了煤层及顶底板样品,利用粉末X射线衍射仪对样品进行了矿物类别分析,利用X射线荧光光谱仪对样品进行了主量元素分析,利用电感耦合等离子体质谱仪对样品进行了微量元素分析.实验结果表明样品中的主要矿物包括高岭石、石英、伊利石、黄铁矿、锐钛矿、金红石、方解石、白云石、钠云母和钠长石等.含量较多的主量元素氧化物为SiO2、TiO2、Al2O3和Fe2O3,存在富集的微量元素为Li、Nb、Ta、Zr、Hf、Sn、Th和In,其中Li、Nb和Ta的含量分别为世界煤均值的7.9倍、7.8倍和8.7倍.沉积物源和矿物赋存特征分析表明,峨眉山中性火山岩和高钛玄武岩对含煤盆地的物质供应具有一定的贡献,沉积之后的热液活动对该煤层关键金属的富集具有重要作用.
Characteristics and genetic mechanism of Li-Nb-Ta enrichment in Late Permian coal in the coalfield of northwestern Guizhou,Southwest China
Critical elements area class of metals that are essential for modern technology but facing supply chain risks. Coal often exhibits enrichment in critical elements due to its high organic matter content,leading to the formation of coal-type critical element deposits under specific geological conditions. Many studies have demonstrated the enrichment of various critical elements in the Late Permian coal-bearing strata of Southwest China. However,the enrichment characteristics and formation mechanisms of these deposits are still unclear.This study focuses on the 9# coal seam of the Late Permian Longtan Formation in the Tailai coal mine,northwestern Guizhou. Systematic sampling of the coal seam,roof,and floor rocks was carried out to characterize the mineralogical and geochemical composition of the deposit. Mineral identification was performed using X-ray diffraction (XRD),while major and trace element analyses were carried out using X-ray fluorescence spectrometry (XRF) and an inductively coupled plasma-mass spectrometer (ICP-MS),respectively. XRD analysis revealed the predominance of kaolinite,quartz,illite,pyrite,anatase,rutile,calcite,dolomite,paragonite,and albite in the samples. Major oxide constituents include SiO2,TiO2,Al2O3,and Fe2O3. The trace elements Li,Nb,Ta,Zr,Hf,Sn,Th,and In exhibit significant enrichment. Concentrations of Li,Nb,and Ta exceed the world coal average by 7.9,7.8,and 8.7 times,respectively. Provenance analysis,coupled with an examination of mineral occurrence characteristics,suggests that medium volcanic rocks and high-Ti basalts sourced from the Emeishan region contributed to the material supply of the marine coal-bearing basin. Furthermore,post-depositional hydrothermal activity is inferred to have played a crucial role in the enrichment of critical elements in the 9# coal seam.

coalfield of northwestern GuizhouLate Permian coalscritical elementsLi-Nb-Ta enrichment

金超、刘浪涛、张小刚、高帅坡、程智伟、李斌斌、周进伟、陈永龙

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河北省资源勘测研究重点实验室,河北邯郸,056038

河北工程大学地球科学与工程学院,河北邯郸,056038

黔西北煤田 晚二叠世煤 关键金属元素 Li-Nb-Ta富集

国家自然科学基金重大研究计划培育项目河北省高等学校科学技术研究重点项目

92162105ZD2022130

2024

地质学报
中国地质学会

地质学报

CSTPCD北大核心
影响因子:2.17
ISSN:0001-5717
年,卷(期):2024.98(8)
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