首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Characterization of primary geochemical haloes for gold exploration at the Huanxiangwa gold deposit, China
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Characterization of primary geochemical haloes for gold exploration at the Huanxiangwa gold deposit, China

机译:Hua香洼金矿床金矿勘探主要地球化学晕的特征

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Recognition of primary geochemical haloes is one of the most important tools for exploring undiscovered mineral resources. This tool is being routinely applied in exploration programs at the Huanxiangwa gold deposit, Xiong'er Mountains, China. Sampling of unweathered rock for multi-element analysis has been undertaken in all completed and ongoing exploration and development work, including drilling and galleries. Samples have been analyzed for 12 elements (Au, Ag, Pb, Zn, Cu, Mo, As, Sb, Bi, Co, Ni and Ba) from unaltered andesites, altered andesites, altered rocks and mineralized altered rocks. To identify multi-element geochemical associations that can be used to recognize enrichment zones, the lithogeochemical datasets were subjected to centered log-ratio transformation to address the closure problem with compositional data, and the log-ratio transformed datasets were subjected to principal components analysis. Results of analyses show that, in the Huanxiangwa deposit, gold mineralization is characterized by a Au±Ag±Cu association, base-metal mineralization by a Zn-Pb-Ag-Cu±As±Sb±Mo association, supra- and/or near-ore primary haloes in mineralized altered rocks by an As±Sb±Bi±Ag±Au±Pb association, sub-ore primary haloes in altered andesites and altered rocks around gold mineralization by a Mo-Bi±Sb±Ba±Zn±Ag association, and the host andesites by a Ni-Co-Ba association. Analyses of axial and longitudinal primary haloes indicate that gold mineralization is overprinted base-metal mineralization in the western and deeper parts of the Huanxiangwa deposit. Modified enrichment indices for Au and linear Au productivity values also indicate extension of gold mineralization with base-metal overprint beneath the western parts of the deposit. Based on this, an exploration target zone extending ca. 200 m below the known ore body was delineated, in which the presence of gold mineralization has been successfully verified by drilling. This study concludes that characterization of primary geochemical haloes associated with known deposits, coupled with analysis of linear element productivities, facilitates vectoring toward ore. Characterization of primary haloes associated with known deposits using lithogeochemical data would benefit highly from applications of log-ratio transformations developed for compositional data analysis.
机译:识别主要的地球化学晕环是探索未发现的矿产资源的最重要工具之一。该工具通常在中国熊耳山环乡洼金矿的勘探计划中使用。在所有已完成和正在进行的勘探和开发工作(包括钻探和画廊)中,已对未风化岩石进行了取样,以进行多元素分析。对样品进行了分析,分析了未改变的安山岩,蚀变的安山岩,蚀变的岩石和矿化的蚀变岩石中的12种元素(金,银,铅,锌,铜,钼,砷,锑,铋,钴,镍和钡)。为了确定可用于识别富集区的多元素地球化学联系,对岩石地球化学数据集进行中心对数比转换,以解决组成数据的封闭问题,并对对数比转换后的数据集进行主成分分析。分析结果表明,在xiang香洼矿床,金矿化特征为Au±Ag±Cu缔合,贱金属矿化特征为Zn-Pb-Ag-Cu±As±Sb±Mo缔合,超和/或通过As±Sb±Bi±Ag±Au±Pb关联在矿化蚀变岩石中的近矿石原生晕,在安山岩中蚀变的亚矿石原生晕和Mo-Bi±Sb±Ba±Zn±的金矿化前后的岩石蚀变Ag协会和镍钴钴协会的主持安山岩。轴向和纵向原生晕的分析表明,金相矿床是Hua香洼矿床西部和较深部分的重印贱金属矿床。修改后的金富集指数和线性金生产率值也表明,金矿的扩展与矿床西部下方的贱金属叠印有关。基于此,一个延伸约ca的勘探目标区。划定了已知矿体以下200 m的位置,其中已通过钻探成功地证实了金矿化的存在。这项研究得出的结论是,与已知矿床有关的主要地球化学晕环的表征,加上对线性元素生产率的分析,都有助于向矿石的向量化。使用岩石地球化学数据表征与已知矿床有关的原生光环,将得益于为成分数据分析开发的对数比变换的应用。

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