首页|辽西新太古代片麻岩金矿中金与伴生元素的多重分形模型剖析

辽西新太古代片麻岩金矿中金与伴生元素的多重分形模型剖析

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新太古代片麻岩在辽西地区分布面积广阔,其中发育的金矿矿产资源丰富.为了研究辽西地区新太古代片麻岩金矿中共伴生元素对于Au元素成矿的重要性,本文以辽西地区新太古代片麻岩中典型金矿床及矿化点矿体的组合分析数据为样本,运用多重分形理论进行Ag、Cu、Pb、Zn、S元素质量分数与金元素质量分数的相关性分析,进而建立了基于多重分形理论的金与共伴生元素多重分形模型.根据多重分形的拟合分析结果显示,Au、Cu、Pb、Zn和S元素的拟合曲线分布状态均呈明显的下凸型,其均匀程度介于正态分布和指数分布之间,广义分维值均大于1.3,说明它们之间存在明显的相关性.而银元素的拟合曲线分布状态明显不同于其它元素,说明银元素的富集不受或受到其它元素的影响很小.结合元素亲和性特征,以硫元素为核心,分析了 Au、Ag、Cu、Pb、Zn的亲硫性,并将新太古代片麻岩金矿中金的演化过程划分成四个阶段,分别为①黄铁矿富集阶段,②自然金伴生阶段,③交代充填阶段,④变质氧化阶段.根据多重分形模型的拟合分析结果,并结合前人的理论研究成果表明:新太古代片麻岩金矿中共伴生元素组合对于金元素成矿极为重要,它为后期找矿的方向及隐伏矿床的发现提供了重要的指示.
Multifractal model analysis of gold and associated elements of Neoarchean gneiss type gold deposit in West Liaoning,China
Neoarchean Gneiss is widely distributed in West Liaoning,where the developed gold mineral re-sources are richful.In order to study the importance of co-associated elements of gold deposits in Neoarchean gneiss in West Liaoning Province for gold mineralization.This article takes the combination analysis data of typical gold deposits and ore bodies in mineralization point within the Neoarchean gneiss in Western Liaoning region as the sample,and applies the multifractal theory to analyze the correlation between the mass fraction of Ag,Cu,Pb,Zn,S elements and Au element.Furthermore,a multifractal model of Au and co-associated elements based on the multifractal theory is established.According to the fitting analysis result of multifrac-tal model,the fitting curve distribution of Au,Cu,Pb,Zn and S elements is obviously downward convex,and their evenness is between Normal distribution and Exponential distribution.The generalized fractal di-mension values are greater than 1.3,indicating that there is an obvious correlation between them.The fit-ting curve distribution state of Ag element is significantly different from other elements,suggesting that the enrichment of Ag element is not affected or is very little affected by other elements.Combined with the char-acteristics of element affinity,the sulfur affinity of Au,Ag,Cu,Pb,Zn is analyzed with S element as the core,and the evolution process of Au in Neoarchean gneiss type gold deposits is divided into four stages,which are ① pyrite enrichment stage,② associated stage of natural gold,③ the stage of replacement and filling and ④ metamorphic oxidation stage,respectively.According to the fitting analysis results of multi-fractal model,combined with the theoretical study result of previous researchers,it is shown that the co-as-sociation of associated elements in Neoarchean gneiss type gold deposits is very important for the gold miner-alization,which can provide an important indicator for the direction of later exploration and prospecting work and discovery of the concealed deposit.

Neoarchean gneissmultifractionsulfur affinityevolutionary process

石娴、李猛猛、李壮

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桂林航天工业学院计算机科学与工程学院,广西桂林 541004

辽宁省化工地质勘查院有限责任公司,辽宁锦州 121000

新太古代片麻岩 多重分形 亲硫性 演化过程

广西科技厅中央引导地方发展基金桂林航天工业学院博士、教授基金项目

KX202204801

2024

矿产与地质
桂林矿产地质研究院

矿产与地质

CSTPCD
影响因子:0.42
ISSN:1001-5663
年,卷(期):2024.38(1)
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