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首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Delineation of deep prospecting targets by combining factor and fractal analysis in the Kekeshala skarn Cu deposit, NW China
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Delineation of deep prospecting targets by combining factor and fractal analysis in the Kekeshala skarn Cu deposit, NW China

机译:NW中国Kekeshala Skarn Cu矿床分形分析划分深度勘探目标

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摘要

Three-dimensional visualization, factor analysis, and fractal/multifractal modeling are combined to study the geochemical data of borehole primary halo in the Kekeshala mining area in Northwestern China to screen exploration targets. First, based on the borehole spatial database comprising collar, survey, geology, and sample tables, 3D borehole primary halo samples are extracted. Their 3D block model is then constructed by spatial interpolation. Second, sample factor analysis of the borehole primary halo mainly includes four factors: F1 consists of Ag-Cu-Sn combination, F2 consists of Pb-Zn combination, F3 consists of As-Sb combination, and F4 consists of Mo-W combination. Moreover, 3D geochemical zoning is conducted for the samples. Third, based on the 3D block model of the primary halo, the F1 factor score is further modeled by Concentration-Volume (C-V) fractal model. Furthermore, based on the fractal fitting line's four segments obtained from the inflection points, geochemical barren host rocks, weakly deep prospect, moderately deep prospect, and highly deep prospect are extracted. Results indicate the following: (a) the F1 factor embodies the main metallogenic process or stage, which can be used as a comprehensive indicator of the spatial aggregation of major metallogenic elements in the study area; (b) the C-V fractal model can effectively determine the F1 factor deep prospect threshold of the skarn-Cu deposit in Kekeshala; and (c) the moderately and highly deep prospects of the F1 factor can well reflect the favorable geological conditions of metallogenesis and be used as the basis for delineating the prospecting target. Therefore, the fractal deep prospect of the geochemical F1 factor of the borehole primary halo has a good application effect in deep prospecting and prediction, which can be effectively used to explore the depth and edge of known deposits.
机译:三维可视化,因子分析和分形/多重分族建模相结合,研究了中国西北部克克斯山矿区山坡原发性光环的地球化学数据筛选勘探目标。首先,基于包括衣领,测量,地质和样本表的钻孔空间数据库,提取3D钻孔初级光晕样本。然后通过空间插值构建它们的3D块模型。其次,钻孔初级光晕的样本因子分析主要包括四个因素:F1由Ag-Cu-Sn组合组成,F2由PB-Zn组合组成,F3由AS-SB组合组成,F4由MO-W组合组成。此外,对样品进行了3D地球化学分区。第三,基于初级光环的3D块模型,F1因子评分通过浓度 - 体积(C-V)分形模型进一步建模。此外,基于从拐点获得的分形贴合线,地球化学贫瘠主体岩石,弱深度前景,中度深度深度,高度深度的前景。结果表明以下内容:(a)F1因子体现了主要的成矿过程或阶段,其可作为研究区域中主要成矿元素的空间聚集的综合指标; (b)C-V分形模型可以有效地确定KEKESHALA矽卡岩铜矿的F1因子深度前景阈值; (c)F1因子的中度和高度深度的前景可以很好地反映了良好的金属化地质条件,并被用作描绘勘探目标的基础。因此,钻孔初级光环的地球化学F1因素的分形深度前景具有良好的应用效果在深度勘探和预测中,可以有效地用于探索已知沉积物的深度和边缘。

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