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The anomalies determined using a soil geochemical survey and prospecting model of the Matou gold deposit in Sichuan Province |
LI Jun-Jun, WEI Yu, ZHANG Qing-Song( ), WANG Wei-Hua, LIU Wei, XIANG Liang |
Sichuan Institute of Metallurgical Geology & Exploration,Chengdu 610006, China |
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Abstract The Matou gold deposit is located in the Mianning-Yanyuan strike-slip orogenic belt and is part of the deeply cut Quaternary coverage area and, thus, has limited surface prospecting clues. In this prospecting stage, a comprehensive anomaly area was delineated through the 1:10 000 soil geochemical survey. Then, gold ore bodies were discovered through trenching engineering, indicating excellent prospecting performance. Moreover, this study established a geological-geochemical prospecting model dominated by the HT3 anomaly area by combining the geological and geochemical anomalies in the work area. Finally, the next prospecting direction was proposed.
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Received: 18 August 2021
Published: 27 April 2023
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Geotectonic location map of Matou gold deposit Ⅴ—Qiangtang-Sanjiang orogenic system; Ⅴ1—Yulongtage-Bayankala foreland basin; Ⅴ1-2—Motianling block; Ⅴ1-3—Kekexili-Songpan foreland basin; Ⅴ1-4—Luhuo-Daofu rift basin; Ⅴ1-5—Yajiang residual basin;Ⅴ2—Garz-Litang arc basin system; Ⅴ2-1—Garz-Litang ophiolite melange belt; Ⅴ2-2—Yidun-Shaluli island arc belt; Ⅴ2-3—Miange-Qingdarou arc back basin; Ⅴ3—Zhongza-Zhongdian block; Ⅴ4—Xijin Ulan lake-Jinsha river-Ailao mountain junction; Ⅴ5—Xichang-Lanping block; Ⅴ5-1—Zhiduo-Jiangda-Weixi continental margin arc belt; Ⅴ5-3—Changdu-Lanping Mesozoic bi-directional back arc foreland basin; Ⅷ—Yangtze block area; Ⅷ1—upper Yangtze block; Ⅷ1-1—passive marginal basin on the western margin of Yangze block; Ⅷ1-2—Yanyuan-Lijiang Mesozoic marginal depression belt; Ⅷ1-3—Chuxiong Mesozoic foreland basin; Ⅷ1-4—Kangding basement complex belt; Ⅷ1-5—east Yunnan Carbonate platform; Ⅷ1-6—west Sichuan foreland basin;1—primary tectonic line;2—secondary tectonic line;3—tertiary tectonic line;4—location of working area
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元素 | 背景值 | 变异系数 | 富集系数 | 中国土壤元 素丰度值[13-14] | Cu | 70.0 | 1.36 | 4.83 | 24 | Pb | 34.7 | 6.56 | 3.77 | 23 | Zn | 115.4 | 1.46 | 2.08 | 68 | As | 29.2 | 1.92 | 11.47 | 10 | Sb | 3.80 | 6.16 | 33.12 | 0.8 | Bi | 0.49 | 1.78 | 3.16 | 0.3 | Hg | 0.178 | 5.31 | 0.03 | 0.04 | Sn | 2.6 | 0.37 | 1.30 | 2.5 | Ag | 0.662 | 2.99 | 16.87 | 0.08 | Au | 7.6 | 4.77 | 41.30 | 1.4 |
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Geochemistry parameters of Matou gold deposit
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地层 | 样本数 | 最小值/10-9 | 平均值/10-9 | 最大值/10-9 | 标准离差 | 变异系数 | 全区 | 2081 | 0.3 | 32.9 | 3580.0 | 153.5 | 4.66 | 峨眉山组 | 3 | 0.8 | 1.1 | 1.6 | 0.3 | 0.31 | 阳新组二段 | 72 | 0.5 | 2.4 | 8.4 | 1.6 | 0.63 | 阳新组一段 | 613 | 0.3 | 41.5 | 3480.0 | 189.7 | 4.57 | 曲靖组二段 | 681 | 0.8 | 10.9 | 438.0 | 24.9 | 2.28 | 坡脚组二段 | 530 | 1.2 | 40.3 | 3580.0 | 178.8 | 4.43 | 辉绿岩 | 182 | 0.7 | 76.9 | 2470.0 | 218.0 | 2.84 |
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Distribution characteristics of Au in soil measurements in main geological bodies
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元素 | 样本数 | 算术平均值 | 标准离差 | 异常下限(外带) | 异常下限(中带) | 异常下限(内带) | Cu | 2087 | 70.0 | 31.8 | 133.7 | 267.4 | 534.8 | Pb | 1954 | 34.7 | 14.7 | 64.2 | 128.4 | 256.8 | Zn | 2064 | 115.4 | 52.8 | 221.1 | 442.2 | 884.4 | As | 1966 | 29.2 | 25.9 | 80.9 | 161.8 | 323.6 | Sb | 1846 | 3.80 | 2.77 | 9.34 | 18.68 | 37.36 | Bi | 2095 | 0.49 | 0.20 | 0.89 | 1.78 | 3.56 | Hg | 2037 | 177.99 | 88.14 | 354.28 | 708.56 | 1417.12 | Sn | 2134 | 2.6 | 0.6 | 3.9 | 7.8 | 15.6 | Ag | 2025 | 0.662 | 0.410 | 1.482 | 2.964 | 5.928 | Au | 1768 | 7.6 | 5.6 | 18.8 | 37.6 | 75.2 |
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List of lower limits of soil anomalies
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元素 | Cu | Pb | Zn | As | Sb | Bi | Hg | Sn | Ag | Au | Cu | 1 | | | | | | | | | | Pb | 0.8146 | 1 | | | | | | | | | Zn | 0.8045 | 0.8279 | 1 | | | | | | | | As | 0.6481 | 0.6544 | 0.6686 | 1 | | | | | | | Sb | 0.5993 | 0.7145 | 0.7806 | 0.7667 | 1 | | | | | | Bi | 0.4072 | 0.262 | 0.3154 | 0.2728 | 0.4432 | 1 | | | | | Hg | 0.6629 | 0.8006 | 0.7353 | 0.7234 | 0.8762 | 0.252 | 1 | | | | Sn | 0.473 | 0.3904 | 0.2432 | 0.3798 | 0.3705 | 0.6486 | 0.478 | 1 | | | Ag | 0.8911 | 0.8502 | 0.7975 | 0.6577 | 0.6758 | 0.3271 | 0.6917 | 0.3314 | 1 | | Au | 0.6685 | 0.6887 | 0.707 | 0.8366 | 0.7843 | 0.3825 | 0.793 | 0.4204 | 0.6989 | 1 |
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Matrix of correlation coefficients of each element of soil geochemistry in Matou gold mining area
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Tree diagram of R-type cluster analysis in soil measurement
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HT1 composite anomaly profile 1—schist of the second member of Yangxin formation;2—limestone of the first member of Yangxin formation;3—limestone of the second member of the Qujing formation;4—calcareous dolomite and limestone of the first member of the Qujing formation;5—carbonaceous slate of the second member of Pojiao formation;6—diabase;7—geologic boundary;8—fault and attitude;9—exploratory trench and numbers;10—industrial ore bodies and numbers;11—low-grade ore bodies and numbers
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HT2 composite anomaly profile 1—schist of the second member of Yangxin formation;2—limestone of the first member of Yangxin formation;3—limestone of the second member of the Qujing formation;4—carbonaceous slate of the second member of Pojiao formation;5—diabase;6—geologic boundary;7—fault and attitude;8—exploratory trench and numbers
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HT3 composite anomaly profile 1—basalt of Emeishan formation;2—schist of the second member of Yangxin formation;3—limestone of the first member of Yangxin formation;4—limestone of the second member of the Qujing formation;5—carbonaceous slate of second member of Pojiao formation;6—diabase;7—geologic boundary;8—fault and attitude;9—exploratory trench and numbers;10—industrial ore bodies and numbers;11—low-grade ore bodies and numbers
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综合异 常编号 | 矿体 编号 | 走向延 伸/m | 平均 厚度/m | Au平均品 位/10-6 | 备注 | HT3 | 1 | 510 | 3.91 | 2.14 | TC00、TC01-1、TC02-1三条探槽控制 | HT3 | 2 | 80 | 0.87 | 1.43 | TC02-1单工程控制 | HT3 | 3 | 80 | 0.87 | 1.32 | TC02-1单工程控制 | HT3 | 4 | 510 | 1.5 | 2.41 | TC00、TC02-1两条探槽控制 | HT3 | 5 | 100 | 0.84 | 5.00 | LD11、LD12两个老硐控制 | HT1 | 6 | 360 | 0.98 | 3.03 | TC07、TC08两条探槽控制 | HT1 | 7 | 360 | 0.98 | 1.80 | TC07、TC08两条探槽控制 |
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Brief description of orebody characteristics
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地球化学剖面线号 | 元素 | 异常重心值/m | 46线 | Cu | 13.23 | Pb | 10.44 | Zn | 8.13 | As | 11.01 | Sb | 15.09 | Bi | 24.27 | Hg | 18.30 | Sn | 101.10 | Ag | 18.69 | Au | 11.88 |
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HT3 composite anomaly map 1—abnormal range and concentration zoning of As;2—abnormal range and concentration zoning of Au;3—abnormal range and concentration zoning of Bi;4—abnormal range and concentration zoning of Sn;5—abnormal range and concentration zoning of Ag;6—abnormal range and concentration zoning of Cu;7—abnormal range and concentration zoning of Hg;8—abnormal range and concentration zoning of Pb;9—abnormal range and concentration zoning of Sb;10—abnormal range and concentration zoning of Zn
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要素类别 | 要素名称 | 要素条件 | 地质 | 地层 | 阳新组一段(P2y1)灰岩为工作区主要赋矿围岩之一,其次在坡脚组板岩(D1pj2)板岩内亦存在矿化现象 | 构造 | 马头山断裂F1及其两侧平行次级裂隙,特别是西侧产于阳新组灰岩内次级裂隙,为主要控矿构造 | 岩浆岩 | 侵入于阳新组中的辉绿岩本身为工作区主要赋矿岩石之一 | 围岩蚀变 | 褐铁矿化、黄铁矿化、绢云母化、硅化带为近矿围岩蚀变 | 矿化种类 | 金 | 地球化学 | 异常形态 | 呈NNE向长轴状带状分布,长宽比约4:1 | 分布特征 | 异常主要沿F1断裂及其两侧呈NNE向发育;平面上,至矿体由远及近分别形成Sn-Bi(外带)、Ag-Hg-Sb(中带)、Cu-Au-As-Pb-Zn(内带)的水平分带现象 | 异常元素特征 | 以Au-As-Sb-Pb-Hg-Ag等中低温多元素组合异常为特征,各元素相互套合较好,峰值高,其中含量达数百乃至数千ppb级别者往往能发现工业矿体,且具有三级浓度分带,浓集中心明显;Bi、Sn元素异常相对较弱 | 剥蚀程度 | 代表中偏低温元素为主的Au、As、Sb、Ag等分布范围广、含量高,代表中及高温元素为主的Sn、Bi分布范围小或者尚未出露,推测异常引起的矿化体剥蚀程度较浅 |
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Geology geochemistry ore forming factors of Matou gold deposit
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Sketch map of geology-geochemistry prospecting model in Matou gold mining area 1—second member of Yangxin formation;2—the first member of Yangxin formation;3—the second member of Qujing formation;4—the first member of Pojiao formation;5—diabase;6—gold orebody;7—limonization;8—pyrite mineralization;9—sericitization;10—silicification;11—geologic boundary;12—major faults and their numbering
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