晋南地区煤系黏土岩中锂的赋存状态及其沉积环境
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本文为国家自然科学基金项目(编号 42172043)和中央高校基本科研业务费专项资金 (编号300102263301)联合资助的成果


Lithium occurrence state and sedimentary environment of clay rocks in coal- bearing strata in southern Shanxi
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    摘要:

    关键金属锂等战略资源及其引发的国家安全问题,在当今国际政治、经济、军事舞台中愈显突出和重要。华北克拉通是我国沉积型锂矿床主要分布区域之一,富锂黏土岩资源丰富,成为重要的沉积型锂资源勘探区域。本文以华北克拉通晋南地区的煤系黏土岩为研究对象,利用X射线粉末衍射(XRD)、X射线荧光光谱(XRF)、电感耦合等离子体质谱(ICP- MS)、傅里叶变换红外光谱(FTIR)和魔角旋转固体核磁共振谱(MAS NMR)等表征技术,结合化学物相分析及黏土矿物分离提取实验对研究区本溪组黏土岩中锂的赋存状态及其沉积环境进行研究。发现黏土矿物是锂的主要载体矿物,其主要包括锂绿泥石、伊利石和高岭石;锂含量与锂绿泥石含量呈显著正相关关系,与伊利石和高岭石的含量呈微弱的正相关关系;样品中的锂主要赋存于锂绿泥石的氢氧化物八面体晶格中,部分赋存于伊利石和高岭石中。古盐度指标m值(100×(MgO/Al2O3))和1000×Rb/K2O值显示研究区富锂黏土岩主要形成于淡水—半咸水环境;古氧化还原指标V/(V+Ni)和Th/U值显示研究区富锂黏土岩主要形成于缺氧和贫氧环境;古气候指标Sr/Cu、C值((V+Cr+Mn+Fe+Co+Ni)/(Na+Mg+K+Ca+Sr+Ba))和CIA值显示研究区富锂黏土岩主要形成于炎热潮湿的古沉积环境中。该研究有助于完善沉积型锂矿的成矿理论,也有利于攻克该类型锂资源高效分离与提取的技术瓶颈。

    Abstract:

    The strategic importance of key metals, such as lithium, and their implications for national security are gaining prominence in the contemporary geopolitical landscape. The North China Craton, with its abundant lithium- rich clay rock resources, represents a significant exploration target for sedimentary lithium deposits in China. This article focuses on the clay rocks in coal- bearing strata in the southern Shanxi area of the North China Craton. A comprehensive suite of characterization techniques, including X- ray powder diffraction (XRD), X- ray fluorescence spectroscopy (XRF), inductively coupled plasma- mass spectrometry (ICP- MS), Fourier transform infrared spectroscopy (FTIR), and magic angle spinning nuclear magnetic resonance spectroscopy (MAS NMR), was employed to investigate the lithium distribution and sedimentary environment of Benxi Formation clay rocks. These techniques are complemented by chemical phase analysis and clay mineral flotation experiments. Results demonstrate that clay minerals are the main carriers of lithium, including Li- chlorite, illite, and kaolinite. A strong positive correlation exists between lithium content and Li- chlorite content, while weaker positive correlations are observed with illite and kaolinite content. Lithium in samples mainly exists in the octahedral lattice of interlayer hydroxide sheets in Li- chlorite, with lesser amounts occurring in illite and kaolinite. Paleoenvironmental indicators, including salinity proxies \[m(100×(MgO/Al2O3)) and 1000×Rb/K2O values\] and redox proxies \[V/(V+Ni) and Th/U values\], suggest that the lithium- rich clay rocks formed in a freshwater to brackish water environment, characterized by anoxic and oxygen- poor conditions. Geochemical proxies, including Sr/Cu, C ((V+Cr+Mn+Fe+Co+Ni)/ (Na+Mg+K+Ca+Sr+Ba)), and CIA values, indicate a hot and humid paleoclimate during their formation. This study contributes to a better understanding of the formation processes of sedimentary lithium deposits and provides valuable insights for developing efficient separation and extraction techniques of this type of lithium resource.

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程宏飞,武振晓.2024.晋南地区煤系黏土岩中锂的赋存状态及其沉积环境[J].地质学报,98(8):2395-2408.
CHENG Hongfei, WU Zhenxiao.2024. Lithium occurrence state and sedimentary environment of clay rocks in coal- bearing strata in southern Shanxi[J]. Acta Geologica Sinica,98(8):2395-2408.

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  • 收稿日期:2024-04-02
  • 最后修改日期:2024-04-22
  • 录用日期:2024-06-09
  • 在线发布日期: 2024-06-20