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The application of geo-electrochemical methods to prospecting in the loess-covered Xiaoshan Mountain, western Henan Province: A case study of the Shilongshan gold polymetallic ore prospecting area in Luoning County |
Xiao-Xiao YANG1, Xian-Rong LUO1, Mei-Lan WEN1, Fei OU-Yang1, Xing-Hai LYu2, Gao-Ke YIN2, Guang-Ming ZHENG2 |
1. College of Earth Sciences,Guilin University of Technology, Guilin 541004,China 2. The Fourth Geological Exploration Institute of Henan Geology and Mineral Bureau, Zhengzhou 450001,China |
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Abstract Xiaoshan Mountain widely covered by the Quaternary sediments is located in the west of Henan Province. Its north part is ravines crossbar, and the surface vegetation grows fully and covers the surface heavily. In order to investigate the effectiveness of the earth electrochemical method in the search for gold deposits in the Xiaoshan loess-covered area in western Henan, the authors selected Shizhaigou gold deposit which is buried in loess to carry out the feasibility test of ore prospecting, and conduct geo-electrochemical prospecting in the south of the Shillongshan gold polymetallic mineral survey area and its adjacent area of Xiaoshan. The study revealed that the electrochemical composite anomaly in the development area of the Au deposit in Shizhaigou is obvious , the elements are well correlated and they have good nesting and zoning relationships. The authors analyzed the trace element content characteristics (fractal, coefficient of variation and extraction ratio of the geoelectric extraction) extracted from the geoelectricity of Shilongshan census area and found that it has similar geoelectricity anomaly patterns to the Shizhaigou gold deposit. In addition, the authors used Surfer software to draw the contour abnormal map and, in combination with previous research results, initially verified the surface of well-arranged 45-47 surveying points along No.02 line through surface engineering, thus determining an industrial gold orebody with good reserves. It is thus proved that the measured and inferred faults F1-1 and F20 do exist. The results provide a theoretical basis for electrochemical prospecting in the search for deep deposits in the Shilongshan area and the periphery of the Shizhaigou deposit, and also provide new ideas for the prospecting work in the loess-covered loess area.
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Received: 21 October 2018
Published: 10 April 2019
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Geological sketch map of the Xiaoshan Mountain in the west of Henan Province(modified according to references [19],[42]) a—geological map of the study area;b—regional structure map;c—distribution of deposits in the study area
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成矿特征要素 | 石寨沟 | 金鸡山 | 申家窑 | 矿床规模 | 小型 | 小型 | 小型 | 矿床类型 | 构造蚀变岩型 | 构造蚀变岩型 | 构造蚀变岩型 | 控矿地层 | 中元古界长城系熊耳群中下部的许山组及马家河组 | 中元古界长城系熊耳群中下部的许山组及马家河组 | 太华群变质岩系 | 控矿构造 | NW-NWW 向、NE-NEE 向及近 SN向,其中 NW-NWW 向和NE-NEE 向断裂为主要含矿断裂 | NW、NE和近SN向断裂,其中NE向断裂破碎带是区内主要的容矿构造 | 矿体受NW-NNW向韧性拆离断层及叠加在其之上的脆性正断层控制,多沿断裂带产出 | 控矿岩体 | 燕山晚期花岗闪长岩、花岗斑岩 | 燕山晚期花岗斑岩、花岗闪长岩 | 燕山晚期花岗斑岩 | 矿石矿物成分 | 主要有自然金、黄铁矿、闪锌矿、方铅矿、黄铜矿 | 主要有自然金、银金矿、黄铁矿、黄铜矿、方铅矿、闪锌矿、菱铁矿及微量的黑钨矿、白钨矿、毒砂 | 黄铁矿最为常见,部分矿石样品中方铅矿有大量产出。其他金属矿物还有毒砂、黄铜矿、闪锌矿以及少量金、银矿物 | 脉石矿物成分 | 石英、绢云母、绿泥石、钾长石、铁白云石 | 石英、绢云母、白云石、钾长石、黑云母、重晶石、绿帘石、锆石 | 石英、菱铁矿,局部可见绢云母 | 矿石结构构造 | 自形—半自形结构、他形粒状结构、压碎结构、包含结构,块状构造、角砾状构造、浸染状构造 | 自形晶、半自形晶、它形晶粒状结构,块状构造、条带状构造、浸染状构造和晶洞状构造 | 自形—半自形粒状结构、他形结构、拔丝结构、压碎结构、揉皱结构为主,条带状、网脉状、团块状和晶洞构造 | 围岩蚀变 | 硅化、绢云母化、黄铁绢英岩化、碳酸盐化、绿泥石化 | 硅化、黄铁矿化、方铅矿化、绿泥石化、绢云母化、泥化 | 硅化、黄铁绢英岩化、碳酸盐化,部分绿泥石化和少量高岭土化 | 矿床有益组分 | Au、Cu、Pb、Zn | Au、Ag、Cu、Pb、Zn | Au、Ag、Cu、Pb、Zn、As |
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Geological characteristics of the main gold deposits
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元素 | 背景值 | 异常 宽度 | 异常 强度 | 异常点号范围 | 峰值 测点 | 异常 峰值 | 异常 形状 | 对应矿体、地质状况 | Au | 2 | 180 | 14.54 | 6、12、13、18~22 | 12 | 36.53 | 单峰 | F7金矿带、 F6含金矿化带 | Ag | 0.03 | 220 | 0.04 | 1~3、13~15、20~22 | 13 | 0.034 | 波状 | F7金矿带、 F6含金矿化带 | Cu | 16 | 180 | 30.81 | 8~13、19、22 | 9 | 2171 | 双峰 | F6、 F7金矿带(有钻孔数据) | Pb | 21 | 340 | 108.05 | 12~19、20~24 | 12 | 347.7 | 单峰 | F7金矿带、 F6含金矿化带 | Zn | 33 | 360 | 56.42 | 2~4、12~23 | 13 | 133.10 | 梯形 | F7金矿带、 F6含金矿化带 | Cr | 12 | 340 | 18.31 | 1~4、12~21 | 17 | 26.60 | 多峰 | F7金矿带、 F6含金矿化带 | Co | 4 | 340 | 5.24 | 1~4、12~21 | 4 | 7.33 | 多峰 | F6、 F7含金矿化带或深部隐伏矿体 | Ni | 18 | 340 | 20.76 | 1~4、12~21 | 4 | 27.96 | 多峰 | F6、 F7含金矿化带或深部隐伏矿体 | Li | 17 | 340 | 19.74 | 1~4、12~21 | 4 | 25.72 | 多峰 | F6、F7含金矿化带或深部隐伏矿体 | As | 5 | 400 | 6.38 | 1~6、12~22 | 4 | 7.80 | 多峰 | F6、 F7含金矿化带或深部隐伏矿体 | Bi | 0.15 | 340 | 0.17 | 1~4、12~21 | 21 | 0.217 | 多峰 | F6金矿带边缘(有探槽TC605) | Ba | 90 | 340 | 102.67 | 1~4、12~21 | 4 | 142.60 | 多峰 | F6、 F7含金矿化带或深部隐伏矿体 | La | 12 | 320 | 14.74 | 1~4、13~21 | 4 | 19.71 | 多峰 | F6、 F7含金矿化带或深部隐伏矿体 | Zr | 11 | 340 | 13.99 | 1~4、12~21 | 4 | 17.04 | 多峰 | F6、 F7含金矿化带或深部隐伏矿体 |
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Geoelectric extraction anomaly parameters of the test section
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Geoelectrochemical anomaly characteristics of the test section
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Elemental fractal statistical graphs of geoelectric extraction measurements
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微量 元素 | 极大值 | 极小值 | 标准 偏差 | 平均值 | 变异 系数 | 陆壳 丰度[38] | 提取比 | 分维数 | 背景值 | D1 | D2 | D3 | Li | 26.44 | 0.20 | 6.13 | 7.17 | 0.85 | 24.1 | 0.30 | 0.258 | 1.597 | 5.091 | 6.92 | Cr | 29.90 | 1.21 | 6.51 | 8.84 | 0.77 | 102 | 0.09 | 0.425 | 1.420 | 3.848 | 7.76 | Co | 11.32 | 0.61 | 1.97 | 2.75 | 0.72 | 23.7 | 0.12 | 0.550 | 1.689 | 4.297 | 2.65 | Ni | 29.29 | 0.61 | 7.06 | 10.01 | 0.71 | 93.6 | 0.11 | 0.261 | 1.509 | 6.588 | 8.32 | Cu | 403.80 | 0.45 | 23.24 | 10.98 | 2.12 | 53.6 | 0.20 | 0.416 | 1.887 | — | 8.51 | Zn | 85.55 | 2.24 | 13.86 | 19.82 | 0.70 | 75.5 | 0.26 | 0.375 | 1.319 | 4.705 | 16.98 | As | 10.22 | 1.21 | 1.74 | 4.03 | 0.43 | 2.29 | 1.76 | 0.969 | 4.516 | — | 4.68 | Zr | 21.61 | 0.33 | 4.94 | 6.19 | 0.80 | 204 | 0.03 | 0.277 | 1.543 | 5.402 | 5.75 | Ag | 0.109 | 0.006 | 0.01 | 0.03 | 0.42 | 0.052 | 0.58 | 0.648 | 4.400 | — | 0.026 | Ba | 188.60 | 1.63 | 34.97 | 42.79 | 0.82 | 449 | 0.10 | 0.199 | 0.793 | 3.671 | 23.44 | La | 21.32 | 0.22 | 4.88 | 5.84 | 0.84 | 34.1 | 0.17 | 0.310 | 1.417 | 4.131 | 5.62 | Au | 49.91 | 0.051 | 3.90 | 3.78 | 1.03 | 1.42 | 2.66 | 0.168 | 1.108 | 2.685 | 1.86 | Pb | 205 | 1.53 | 22.28 | 15.81 | 1.41 | 14.2 | 1.11 | 0.649 | 1.481 | — | 13.24 | Bi | 0.59 | 0.004 | 0.06 | 0.08 | 0.81 | 0.586 | 0.30 | 0.304 | 2.377 | 7.599 | 0.09 |
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Elemental statistics of geoelectric extraction measurements
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Distribution of geoelectric extraction lines in the Shilongshan research area
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Geoelectric extraction element F1、F2 assemblage anomaly map
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Engineering verification cross-section of Shilongshan research area
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