河南官坡花岗伟晶岩地质与地球化学特征

    Geological and geochemical characteristics of granitic pegmatite in Guanpo, Henan Province

    • 摘要: 河南省官坡镇境内出露大量花岗伟晶岩脉,部分花岗伟晶岩脉发育稀有金属或稀有多金属矿化,具有稀有金属找矿潜力和研究价值。通过野外地质调查、岩相学观察和元素地球化学分析,对官坡花岗伟晶岩的特征和成因进行研究。结果显示: 官坡花岗伟晶岩脉具有分布集中、延伸稳定、规模较大、结构带发育完整、物质组成复杂的特点; 花岗伟晶岩主量元素具有高硅、富碱、过铝质及低铁、镁、钙和钛的特点,在成因上可能与灰池子花岗岩具有亲缘性,推测是该花岗岩高度演化后的产物。该研究进一步提高了对该区花岗伟晶岩的研究程度,为区内稀有金属矿勘查提供借鉴。

       

      Abstract: Granitic pegmatite veins outcropped widely and some veins developed rare metal or rare polymetal mineralization in Guanpo of Henan Province, which possess great research value and prospecting potential. The authors researched the features and origins of the granitic pegmatite through field geological survey, petrographic observation and element geochemistry analysis. The results show that granitic pegmatite veins have the characteristics of centralized distribution, relatively stable extension, large scale, completely developed structural belt and complicated mineralogy. The granitic pegmatite veins have high silica content, rich alkali and peraluminous, and they also have low iron, magnesium, calcium and titanium content. They may have good affinity to Huichizi granite in the aspect of origin, and thus the authors speculated that they could be the products of the highly evolved granite. This study further improved the research level of the granitic pegmatite, and provided references for the prospecting of rare metal deposits in the study area.

       

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