陈小浪,张梅梅,唐座,杨星.金沙地区含铝岩系中锂元素富集特征浅析[J].贵州地质,2024,(3):256-269
金沙地区含铝岩系中锂元素富集特征浅析
Analysis on the Enrichment Characteristics of Lithium in Aluminium-bearing Rock Series in Jinsha County
投稿时间:2024-03-08  
DOI:
中文关键词:  金沙县  含铝岩系    地球化学元素  相关性
英文关键词:Jinsha County  Aluminium-bearing Rock Series  Lithium  Geochemical elements  Correlation
基金项目:贵州省威宁地区中二叠统梁山组三稀元素富集特征及其地质因素(黔地矿科合〔2017〕15号)
作者单位
陈小浪 贵州省地矿局区域地质调查研究院贵州贵阳550004 
张梅梅 贵州省地矿局区域地质调查研究院贵州贵阳550004 
唐座 贵州省地矿局区域地质调查研究院贵州贵阳550004 
杨星 贵州省地矿局区域地质调查研究院贵州贵阳550004 
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中文摘要:
      厘清金沙地区下石炭统九架炉组铝质黏土岩系中锂的富集机制,为锂资源的综合利用与评价提供参考依据。文本评价金沙县坪子上和桶井研究区的锂资源经济价值,研究含铝岩系化学元素在平面和垂向上的分布特征,并分析化学元素的相关性。结果表明,坪子上研究区平面上Li2O呈北高南低、桶井研究区呈西北高东南低。垂向上,Li2O含量在1 000×10-61 999×10-6的样品占分析样品总数的1687%、在2 000×10-62 999×10-6的样品占分析样品总数的542%、在>3 000×10-6的锂样品占分析样品总数的181%,Li2O在铝土岩中最为富集,其次为粘土岩、铝土矿。Li2O与Al2O3(r=040)、TiO2(r=043)呈正相关,Li2O与SiO2(r=-033)、TFe2O3(r=-020)呈负相关,Li2O与A/S(铝硅比)(r=004)、岩层厚度(r=-007)无相关关系。
英文摘要:
      To clarify the enrichment mechanism of lithium in the aluminous clay rock series of the Lower Carboniferous Jiujialu Formation in Jinsha area,and provide reference for the comprehensive utilization and evaluation of lithium resourcesThis paper evaluates the economic value of lithium resources in Pingzishang and Bucket Jing research area of Jinsha County,studies the distribution characteristics of chemical elements in horizontal and vertical space of aluminium-bearing rock series,and analyzes the correlation of chemical elementsThe results show that lithium resources in the study area have no industrial valueLithium resources are high in the north and low in the south in the Pingzishang,and high in the northwest and low in the southeast in the TongjingVertically,samples with Li2O content of 1 000×10-61 999×10-6 accounted for 1687% of the total analysis samples,samples with 2 000×10-62 999×10-6 accounted for 542%,and lithium samples with content of >3 000×10-6 accounted for 181%Li2O is the most abundant in bauxite,followed by clay rock and bauxiteLi2O is positively correlated with Al2O3 (r=040) and TiO2 (r=043),negatively correlated with SiO2 (r=-033) and TFe2O3 (r=-020),and has no correlation with A/S (aluminum-silicon ratio) and rock layer thickness
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