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| Geochemical characteristics and anomaly assessments of soils in the Songshunangou gold mining area, Qinghai Province |
CHEN Geng-Hu1( ), LANG Xing-Hai2( ), WANG Zhao-Shuai3, DONG Wei-Cai1, WANG Deng-Ke1, XIANG Zuo-Peng2, LI Zhuang4, YE Zi-Feng2, WU Chang-Yi2, WANG Xu-Hui2, WU Tian-Wen1, LUO Chao1 |
1. Sichuan Xinshun Mining Co., Ltd., Chengdu 610041, China 2. College of Earth and Planetary Sciences, Chengdu University of Technology, Chengdu 610059, China 3. Shandong Geology and Mineral Resources Engineering Group Co., Ltd., Jinan 250013, China 4. College of Greography and Resources Science, Neijiang Normal University, Neijiang 641100, China |
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Abstract The Songshunangou gold mining area in Qinghai Province is situated in the central part of the North Qilian metallogenic/orogenic belt. Two deposits have been identified in its eastern and western portions, with cumulative proven Au resources exceeding 34 t, establishing them as large-scale deposits. Moreover, the area holds significant potential for ore prospecting, necessitating an urgent need for research into prospecting orientations to support mineral exploration efforts. Hence, based on the anomaly analysis of 1∶10 000 soil geochemical survey data and employing the two-window moving average method, this study identified the anomaly distributions and enrichment patterns of 10 elements (i.e., Au, As, Sb, Hg, Cu, Pb, Zn, Ag, W, and Mo) in the area. By analyzing elemental geochemical anomaly data and integrating the geological conditions for mineralization, this study delineated composite anomaly zones in the area using the average contrast method, followed by anomaly assessments. The results indicate that Au is the primary ore-forming element in the area, characterized by strong enrichment and significant variability, suggesting high mineralization potential. Seven composite soil geochemical anomaly zones were delineated in the area, with zones HP-1, HP-2, and HP-5 demonstrating the greatest potential for mineral exploration. Engineering validation confirms the presence of two ore/mineralized bodies, with one exhibiting an ore thickness of 1.5 m and a gold grade of 0.57 g/t in zone HP-2 and the other featuring an ore thickness of 1.42 m and a gold grade of 1.67 g/t in zone HP-5. Overall, this study provides geochemical evidence for determining prospecting orientations in the Songshunangou gold mining area while offering a reference for the deployment of subsequent mineral exploration work in the area.
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Received: 07 April 2025
Published: 30 December 2025
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Corresponding Authors:
LANG Xing-Hai
E-mail: wzs371421@163.com;langxinghai@126.com
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The location of the Songshunangou mining area and its surrounding geological structures (a) and geological map (b)
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Fig.1) ">
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Soil geochemical sampling range dendrogram of the Songshunangou district(the geological sketch is shown in Fig.1)
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| 参数 | Au | Ag | As | Sb | Hg | Cu | Zn | Mo | W | Pb | | 最小值 | 0.18 | 0.71 | 2.52 | 0.28 | 3.6 | 1 | 1.13 | 0.21 | 0.2 | 4.2 | | 中位数 | 1.39 | 72 | 17.9 | 1.15 | 29 | 29.9 | 90.4 | 1.05 | 2.06 | 2.06 | | 最大值 | 720 | 3700 | 1281 | 139 | 1140 | 290 | 870 | 6.58 | 41.4 | 886 | | 平均值 | 2.44 | 76 | 23.99 | 1.42 | 32.22 | 33.93 | 93.43 | 1.06 | 2.11 | 27.9 | | 标准离差 | 9.47 | 49.05 | 27.95 | 1.78 | 24.25 | 14.12 | 23.67 | 0.26 | 0.69 | 21.65 | | 变异系数 | 3.89 | 0.65 | 1.17 | 1.25 | 0.75 | 0.42 | 0.25 | 0.25 | 0.33 | 0.78 | | 克拉克值 | 1.35 | 66.1 | 12.4 | 0.82 | 24.7 | 19.5 | 55.5 | 0.66 | 1.66 | 20.2 | | 浓度克拉克值 | 1.81 | 1.15 | 1.93 | 1.73 | 1.3 | 1.74 | 1.68 | 1.61 | 1.27 | 1.38 |
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Soil geochemical parameter in the Songshunangou district
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Correlation matrix diagram of soil geochemical elements in the Songshunangou district
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Dendrogram of R-type cluster analysis dendrogram of soil geochemical elements in the Songshunangou district
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| 元素 | F1 | F2 | F3 | | Au | 0.576 | -0.026 | 0.048 | | Ag | 0.291 | 0.331 | 0.245 | | As | 0.877 | 0.066 | 0.203 | | Sb | 0.878 | 0.063 | 0.001 | | Hg | 0.102 | 0.490 | -0.524 | | Cu | -0.005 | -0.209 | 0.119 | | Zn | 0.069 | 0.083 | 0.849 | | Mo | 0.067 | 0.734 | 0.075 | | W | -0.037 | 0.711 | 0.143 | | Pb | 0.280 | 0.402 | 0.672 | | 特征值 | 2.054 | 1.616 | 1.591 | | 累积方差贡献率/% | 20.542 | 36.698 | 52.608 |
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Factor analysis results in the Songshunangou district
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| 参数 | Au | As | Sb | Hg | Cu | Pb | Zn | Ag | W | Mo | | 背景值 | 0.11 | 0.43 | 0.03 | 0.57 | 0.64 | 0.40 | 0.26 | 1.04 | 0.01 | 0.01 | | 异常下限 | 0.92 | 5 | 0.3 | 9 | 8 | 6 | 12 | 14 | 0.4 | 0.2 |
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Factor analysis results in the Songshunangou district
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Element anomaly in the Songshunangou district
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Comprehensive anomaly map of soilelements in the Songshunangou district
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| 模型要素 | 要素特征 | 分类 | | 控矿因素 | 构造 | 受NW—SE向构造控制 | 重要 | | 地层 | 主要赋矿地层为上奥陶统扣门子 组,主要赋矿岩性为玄武安山岩、 晶屑凝灰岩及流纹质凝灰岩 | 必要 | | 岩浆岩 | 与成矿有关的岩体为晚奥陶世石 英闪长斑岩 | 必要 | | 找矿标志 | 地球化学 | Au为松树南沟矿区的主要成矿 元素,As、Sb为前缘元素,Ag、Pb、 Zn为近矿元素 | 必要 | | 围岩蚀变 | 斑岩型矿化赋矿蚀变为钾化、青 磐岩化以及绢云母—绿泥石化, 其中钾化蚀变是矿体中心的指示 标志;浅成低温热液型矿化赋矿 蚀变为绢云母—绿泥石化以及 局部的绢英岩化蚀变 | 必要 |
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Mining model in the Songshunangou district
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