喜马拉雅琼嘉岗伟晶岩型锂矿放射性与波谱特征及找矿意义

Radioactive and Spectral Characteristics of the Qiongjiagang Pegmatite-Type Lithium Deposit in the Himalayas and Their Significance of Ore Prospecting

  • 摘要: 锂资源在新能源产业中具有重要地位,其高效勘查直接关系新能源产业链的安全与稳定。伟晶岩型锂矿因资源品位高、易开采,成为锂资源的主要来源之一。琼嘉岗矿区是喜马拉雅成矿带首例具有工业价值的伟晶岩型锂矿,前人已对其地球化学和物理探测方面作了大量研究,但对于该矿区伟晶岩型锂矿的放射性特征与波谱特征方面的研究尚不明确,限制了遥感技术在该矿区的有效应用。本文研究了喜马拉雅琼嘉岗矿区伟晶岩型锂矿的放射性特征与波谱特征,探索适用于该矿区的遥感识别方法,建立一种基于放射性特征与波谱特征的双指标识别方式,以实现对含锂辉石伟晶岩的快速、准确识别。使用环境X、γ辐射测量仪、X射线荧光光谱仪和高光谱地物波谱仪,对琼嘉岗矿区进行野外放射性测量、放射性元素含量测量、室内波谱测试分析及各类岩石矿物成分检测。研究表明,琼嘉岗矿区各类岩石的放射性特征依次为伟晶岩 > 花岗岩 > 围岩(大理岩) > 其他岩石,伟晶岩表现出明显的Th异常。在波谱特征方面,1900、2200、2480~2490 nm波段具有找矿诊断性特征,能够有效区分含锂辉石伟晶岩、无矿伟晶岩及围岩。此外,各类岩石的反射率总体表现为含矿伟晶岩 > 无矿伟晶岩 > 花岗岩 > 围岩(大理岩)。本研究得到琼嘉岗矿区各类岩石放射性特征范围和含矿伟晶岩找矿指示波段,揭示了琼嘉岗矿区伟晶岩型锂矿的放射性特征与波谱特征,提出基于双指标的识别方法,实现了便捷、高效的找矿目标。

     

    Abstract: Lithium resources play a crucial role in the new energy industry, and their efficient exploration is directly related to the safety and stability of the new energy industrial chain. Pegmatite-type lithium deposits have become one of the main sources of lithium resources due to their high resource grade and easy exploitability. The Qiongjiagang mining area is the first pegmatite-type lithium deposit with industrial value in the Himalayan metallogenic belt. Previous researchers have conducted extensive studies on its geochemistry and physical prospecting; however, the current research on the radioactive characteristics and spectral characteristics of the pegmatite-type lithium deposits in this mining area remains unclear, which limits the effective application of remote sensing technology in the mining area. This study investigates the radioactive characteristics and spectral characteristics of pegmatite-type lithium deposits in the Qiongjiagang mining area of the Himalayas, explores remote sensing identification methods applicable to this mining area, and establishes a dual-index identification method based on radioactive characteristics and spectral characteristics to achieve rapid and accurate identification of spodumene-bearing pegmatites. In this study, an environmental X and γ radiation detector, an X-ray fluorescence spectrometer, and a hyperspectral ground object spectrometer were used to conduct field radioactive measurements, radioactive element content measurements, indoor spectral test analysis, and mineral composition detection of various rocks in the Qiongjiagang mining area. Studies have shown that the radioactive characteristics of various rocks in the Qiongjiagang mining area follow the order: pegmatite > granite > surrounding rock (marble) > other rocks, with pegmatite exhibiting obvious thorium (Th) anomalies. In terms of spectral characteristics, the wavebands of 1900 nm, 2200 nm, and 2480-2490 nm possess diagnostic features for ore prospecting, which can effectively distinguish spodumene-bearing pegmatites, non-ore-bearing pegmatites, and surrounding rocks. In addition, the reflectance of various rocks generally follows the sequence: ore-bearing pegmatite > non-ore-bearing pegmatite > granite > surrounding rock (marble). This study has obtained the range of radioactive characteristics of various rocks in the Qiongjiagang mining area and the prospecting indicator wavebands for ore-bearing pegmatites, revealed the radioactive and spectral characteristics of pegmatite-type lithium deposits in the Qiongjiagang mining area, and proposed an identification method based on dual indicators, thereby achieving the goal of convenient and efficient ore prospecting.

     

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