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Characteristics of rock geochemical anomalies and prospecting potential of the Sinongduo silver polymetallic deposit, Tibet |
Zong-Yao YANG1, Chong-Hai ZHANG2, Xiao-Yan ZHAO1( ), Xing-Hai LANG2, Hong-Tian XIAO2, Jun LIANG3 |
1. Faculty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 611756, China 2. College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China 3. Zhongrui Mining Co., Ltd., Lhasa 850000, China |
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Abstract The Sinongduo silver polymetallic deposit is the first low sulfidation epithermal deposit found in the Linzizong volcanic rocks. Its unique origin and metallogenic geological background indicate great prospecting potential of the south Gangdise metallogenic belt. The zoning characteristics of metallogenic elements were studied by means of large scale rock geochemical survey in the Sinongduo deposit. The large coefficient of variation and standard deviation of Pb, Zn, Cd, Ag and Au indicate the high enrichment and enrichment capability of these elements. Cluster analysis shows high correlation between Pb, Zn, Cd, Ag and Au which are considered to be the main mineralization elements. Element anomalies are classified according to the cumulative frequency of 75%, 95% and 98.5% and 2 anomalies area are considered to have high prospecting potential. The authors are in the hope that the data obtained can provide a guide for the geochemical prospecting in the Gangdise metallogenic belt.
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Received: 25 September 2017
Published: 15 August 2019
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Corresponding Authors:
Xiao-Yan ZHAO
E-mail: xyzhao2@swjtu.cn
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Simplified geological map of the Sinongduo silver polymetallic deposit
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参数 | Cu | Pb | Zn | Cd | Mo | Ag | As | Sb | Hg | Au | 样品个数 | 2413 | 2413 | 2413 | 2413 | 2413 | 2413 | 2413 | 2413 | 2413 | 2413 | 最小值 | 1.3 | 7.8 | 10.3 | 0.02 | 0.25 | 0.04 | 1.7 | 0.7 | 4.0 | 0.6 | 最大值 | 403 | 50806 | 21046 | 109 | 67.3 | 120 | 393 | 72.4 | 638 | 305 | 均值 | 12.5 | 127.3 | 88.7 | 0.18 | 2.59 | 0.41 | 31.4 | 2.8 | 32.4 | 2.9 | 标准偏差 | 9.6 | 1300 | 429.6 | 2.22 | 3.57 | 3.44 | 27.8 | 2.6 | 23.6 | 9.8 | 变异系数 | 0.8 | 10.2 | 4.8 | 12.6 | 1.38 | 8.38 | 0.9 | 0.9 | 0.7 | 3.4 | 偏斜 | 29.2 | 30.1 | 48.2 | 48.79 | 8.4 | 26.16 | 5 | 12.5 | 13.3 | 18.7 | 峰度 | 1143 | 1048 | 2351 | 2391 | 111 | 777 | 40 | 262 | 272 | 482 | 累积 频率 | ≤75% | 15.2 | 58.7 | 84.6 | 0.13 | 2.73 | 0.17 | 33.4 | 2.92 | 36 | 1.81 | ≤95% | 17.7 | 125 | 128 | 0.22 | 7.32 | 0.96 | 78 | 5.66 | 54 | 7.31 | ≤98.5% | 19.9 | 500 | 234 | 0.55 | 13.2 | 2.64 | 127 | 9.92 | 73 | 22.3 |
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Geochemical parameter characteristics of various elements in rock survey at the scale of 1:10 000 in the Sinongduo silver polymetallic deposit
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Cluster analysis dendrogram of elements in the Sinongduo silver polymetallic deposit
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Elements distribution model in hydrothermal deposits
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Anomaly map of various elements based on rock geochemical survey in the Sinongduo silver polymetallic deposit
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