北山北带金豹梁铍矿成矿过程元素地球化学指标研究及意义
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1.甘肃省地学大数据工程研究中心;2.甘肃省地质调查院;3.甘肃省矿产资源勘查重点实验室;4.兰州大学地质科学与矿产资源学院

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P536

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国家科技攻关计划,国家重点基础研究发展计划(973计划)


Metallogenic Process and Element Geochemical Indicators of the Jinbaoliang Beryllium Deposit in the Northern Beishan Belt and Their Significance
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1.Geoscience Big Data Engineering Research Center of Gansu Province;2.Geological Survey of Gansu Province;3.Key Laboratory of Mineral Exploration,Gansu Province.;4.Key Laboratory of Mineral Exploration,Gansu Province;5.School of Earth Sciences,Lanzhou University.

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    摘要:

    近年甘肃北山北带发现了金豹梁、乌云淖尔等一批铍铌钽等稀有金属矿点,显示该区稀有金属成矿条件好,找矿潜力大。但目前该区稀有金属矿研究程度很低,特别是对稀有金属富集成矿过程中元素地球化学变化规律尚未开展系统研究。本次通过详细的野外调查和室内综合分析,系统研究了金豹梁铍矿区二长花岗岩铍矿及其围岩和花岗斑岩铍矿及其围岩等不同矿化程度花岗岩的元素地球化学特征,发现Be富集成矿过程中Si、Al、Ti、Nb、Ta、Rb、Li、Cs、Zr、Hf、REE等元素存在规律性变化,总结了Be成矿过程中有效元素地球化学指标,发现两类花岗岩型铍矿元素地球化学特征存在较大差异,表明不是一期岩浆结晶分异产物,即存在两期(或两阶段)两类花岗岩铍成矿;同时发现金豹梁花岗岩型铍矿成矿过程元素地球化学特征与典型花岗岩型铍矿(高分异花岗岩)存在显著差异,表明研究区可能存在稀有金属品位较高的高分异花岗岩,为金豹梁地区铍等稀有金属矿找矿提供了新的思路和方向,为北山北带稀有金属成矿研究和找矿工作提供了依据。

    Abstract:

    In recent years, a series of rare metal occurrences including beryllium, niobium and tantalum deposits such as Jinbaoliang and Wuyunuoer have been discovered in the northern belt of the Beishan Mountains, Gansu Province, indicating favorable metallogenic conditions and great prospecting potential for rare metals in this region. However, the research level on rare metal deposits in this area remains relatively low, and systematic studies on the elemental geochemical variation laws during the enrichment and mineralization of rare metals are particularly lacking. Based on detailed field geological surveys and comprehensive indoor analyses, this study systematically investigates the elemental geochemical characteristics of monzogranite beryllium ore and its surrounding rocks, as well as granite porphyry beryllium ore and its surrounding rocks with varying mineralization degrees in the Jinbaoliang beryllium mining area. Regular variations of elements including Si, Al, Ti, Nb, Ta, Rb, Li, Cs, Zr, Hf and REE are identified during beryllium enrichment and mineralization, and effective elemental geochemical indicators for beryllium mineralization are summarized. Significant differences in elemental geochemical characteristics are recognized between the two types of granite-type beryllium deposits, suggesting that they are not products of a single-stage magmatic fractional crystallization, and verifying the existence of two-stage and two-type granite beryllium mineralization in the study area. Furthermore, the elemental geochemical features of Jinbaoliang granite-type beryllium deposits differ markedly from those of typical highly fractionated granite-type beryllium deposits, implying the potential occurrence of highly fractionated granites with high rare metal grades in the study area. The results provide new insights and directions for the prospecting of rare metal resources such as beryllium in the Jinbaoliang area, and offer a theoretical basis for metallogenic research and exploration of rare metals in the northern Beishan belt.

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吴义布,徐磊,司豪佳,等. 北山北带金豹梁铍矿成矿过程元素地球化学指标研究及意义[J]. 科学技术与工程, , ():

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  • 收稿日期:2026-04-26
  • 最后修改日期:2026-06-15
  • 录用日期:2026-07-27
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