张辰光, 查道函, 刘明华, 周红升, 史兴俊, 严育通, 黄昆. 湖南肖家山金矿床金元素分形特征及地质意义[J]. 信阳师范学院学报(自然科学版), 2019, 32(3): 421-425. DOI: 10.3969/j.issn.1003-0972.2019.03.014
引用本文: 张辰光, 查道函, 刘明华, 周红升, 史兴俊, 严育通, 黄昆. 湖南肖家山金矿床金元素分形特征及地质意义[J]. 信阳师范学院学报(自然科学版), 2019, 32(3): 421-425. DOI: 10.3969/j.issn.1003-0972.2019.03.014
ZHANG Chenguang, ZHA Daohan, LIU Minghua, ZHOU Hongsheng, SHI Xingjun, YAN Yutong, HUANG Kun. Gold Element Fractal Characteristics and Geological Significance of Xiaojiashan Gold Deposit[J]. Journal of Xinyang Normal University (Natural Science Edition), 2019, 32(3): 421-425. DOI: 10.3969/j.issn.1003-0972.2019.03.014
Citation: ZHANG Chenguang, ZHA Daohan, LIU Minghua, ZHOU Hongsheng, SHI Xingjun, YAN Yutong, HUANG Kun. Gold Element Fractal Characteristics and Geological Significance of Xiaojiashan Gold Deposit[J]. Journal of Xinyang Normal University (Natural Science Edition), 2019, 32(3): 421-425. DOI: 10.3969/j.issn.1003-0972.2019.03.014

湖南肖家山金矿床金元素分形特征及地质意义

Gold Element Fractal Characteristics and Geological Significance of Xiaojiashan Gold Deposit

  • 摘要: 湖南省肖家山金矿位于钦杭成矿带湖南段湘东北亚段,成矿条件良好,但其多期多阶段的特征成矿特征制约了区内勘查工作的进行.利用分形理论对肖家山金矿床品位和资源量进行了分析,揭示了分形分维特征与金富集成矿过程的关系,对矿山深边部的找矿具有重要的指导意义.研究表明,金品位分布直方图暗示了成矿过程具有多期矿化叠加特征.金品位具双重分维结构,分别对应着早期成矿预富集的石英―黄铁矿阶段、主要成矿的石英―硫化物阶段,而晚期的石英-铁白云石阶段对成矿并无贡献,反映了矿化的不均匀特征.资源量存在不同区段的多重分形,分维值小于1,表明矿床储量规模的分布差异较大,分布相对比较分散,具有良好的找矿潜力.

     

    Abstract: Xiaojiashan gold deposit is located in Qin-hang metallogenic belt in Hunan provice. The orefield has good metallogenetic conditions. But the multistage metallogenic characteristics of the deposit restrict the exploration in the area. Its gold grade and resource were analyzed using the fractal theory, and the relationship between fractal features and gold enrichment and mineralization process was revealed. It has an important guiding significance to ore prospecting to depth and in surroundings of mines.The results showed that the distribution histogram of gold grade indicates that the mineralization process has the characteristics of multistage mineralization superposition. The gold grade has a double fractal structure and fractal dimension, corresponding to the early ore-preenriched quartz-pyrite stage, the main ore-forming quartz-sulfide stage, late quartz-ferrodolomite stage did not contribute to the mineralization, Which reflects the inhomogeneity of mineralization. There are multiple fractals in different sections of the resource quantity, and the fractal dimension value is less than 1, which indicated that the reserves scale of the deposit varies greatly and the distribution was relatively dispersed. The deposit has good prospecting potential.

     

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