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物探与化探  2021, Vol. 45 Issue (6): 1425-1438    DOI: 10.11720/wtyht.2021.1470
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
相山矿田游坊地区地电提取找矿预测
唐瑞1(), 欧阳菲1(), 罗先熔1, 郑超杰1, 汤国栋1, 刘攀峰1, 蔡叶蕾1, 杨笑笑2
1.桂林理工大学 地球科学学院隐伏矿床预测研究所,广西 桂林 541004
2.广西三一〇核地质大队,广西 桂林 541000
The prediction of electrochemical prospecting in Youfang area of the Xiangshan orefield
TANG Rui1(), OUYANG Fei1(), LUO Xian-Rong1, ZHENG Chao-Jie1, TANG Guo-Dong1, LIU Pan-Feng1, CAI Ye-Lei1, YANG Xiao-Xiao2
1. Institute for Prediction of Hidden Deposits, School of Geosciences, Guilin University of Technology, Guilin 541004,China
2. No.310 Geological Party of Guangxi Zhuang Autonomous Region,Guilin 541000,China
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摘要 

为在江西相山矿田游坊地区实现找矿突破,在该区开展地电提取测量工作进行深部找矿预测。研究发现:异常明显受断裂控制,主要沿控矿断裂及断裂交汇处展布;运用聚类分析和因子分析发现各微量元素之间具有显著相关性,据此得出相应的元素组合:F1因子(Ti-V-Mo-Th-U)、F2因子(As-Pb-Sb)、F3因子(Co-Ni);铀钍比的空间分布与AMT推测基底深度呈现明显正相关关系,推测主要受火山岩厚度的控制。综合地电提取元素异常特征和相山矿田成矿规律,建立综合地质—地电化学找矿模式,并在研究区内圈定出两个相应的靶区,其中1号靶区具有良好找矿前景。
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唐瑞
欧阳菲
罗先熔
郑超杰
汤国栋
刘攀峰
蔡叶蕾
杨笑笑
关键词 ： 相山,  铀矿,  地电提取,  异常特征    
Abstract：

In order to make a breakthrough in prospecting in the Youfang area of the Xiangshan ore field, the authors carried out geoelectric extraction and surveying in this area for deep prospecting prediction. It is found that the anomalies are obviously controlled by the faults, and are mainly distributed along the ore-controlling faults and the intersection of the faults. Cluster analysis and factor analysis reveal that there is a significant correlation between the trace elements, thus forming the corresponding element combinations: F1 factor (Ti、V、Mo、Th、U), F2 factor (As、Pb、Sb), and F3 factor (Co、Ni). The spatial distribution of uranium-thorium ratios shows a significant positive correlation with the estimated base depth of AMT, controlled by volcanic rock thickness. The authors synthesized the abnormal features of geoelectrically extracted elements and the mineralization regularity of the Xiangshan ore field, established a comprehensive geological-geoelectrochemical prospecting model, and delineated two corresponding targets in the study area, of which No.1 target area has good prospecting prospect.
Key words： Xiangshan    uranium ore    geo-electric extraction    characteristics of anomaly
收稿日期: 2020-09-23      修回日期: 2021-01-08      出版日期: 2021-12-20
ZTFLH:  P632  
基金资助:国家重点研发计划“华南热液型铀矿基地深部探测技术示范”(2017YFC0602600);广西教育厅项目(2017KY0239)
通讯作者: 欧阳菲
作者简介: 唐瑞(1995-),男,硕士研究生,主要从事地球化学研究工作。Email: 945087837@qq.com
引用本文:   
唐瑞, 欧阳菲, 罗先熔, 郑超杰, 汤国栋, 刘攀峰, 蔡叶蕾, 杨笑笑. 相山矿田游坊地区地电提取找矿预测[J]. 物探与化探, 2021, 45(6): 1425-1438.
TANG Rui, OUYANG Fei, LUO Xian-Rong, ZHENG Chao-Jie, TANG Guo-Dong, LIU Pan-Feng, CAI Ye-Lei, YANG Xiao-Xiao. The prediction of electrochemical prospecting in Youfang area of the Xiangshan orefield. Geophysical and Geochemical Exploration, 2021, 45(6): 1425-1438.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2021.1470      或      https://www.wutanyuhuatan.com/CN/Y2021/V45/I6/1425
Fig.1  相山盆地地质构造略图(据董保平[25]修改)
1—白垩系上统龟峰群;2—白垩系下统鹅湖岭组;3—白垩系下统打鼓顶组;4—三叠系上统安源组;5—石炭系下统华山岭组;6—新元古界;7—次斑状花岗岩;8—花岗岩;9—实测、推测断层;10—赣杭断裂带;11—赣杭构造带范围;12—红色断陷盆地;13—火山盆地;14—铀矿床;15—相山矿田;16—研究区
Fig.2  游坊研究区地质
Fig.3  地电提取提取迁移模式简图(据罗先熔[27]修改)
Fig.4  64线地质—地化异常综合剖面(据王东[29]修改)
1—第四系;2—白垩系下统鹅湖岭下段;3—白垩系下统鹅湖岭上段;4—白垩系下统打鼓顶组下段;5—白垩系下统打鼓顶组上段;6—新元古界;7—次斑状花岗岩;8—铀矿体;9—空隙;10—断裂;11—点位及点号;12—钻孔及编号
指标 Ti V Co Ni As Cu Zn Mo Sb Pb Th U
算数平均值 4.69 0.37 0.30 0.63 2.41 19.33 0.16 0.01 0.04 3.18 0.20 0.10
中值 3.53 0.31 0.14 0.41 1.06 7.86 0.12 0.01 0.03 1.53 0.17 0.06
众数 2.24 0.26 0.13 0.42 0.58 4.76 0.10 0.01 0.03 1.50 0.15 0.04
标准差 5.20 0.40 0.59 0.68 6.38 42.94 0.27 0.01 0.06 15.28 0.28 0.26
最小值 1.16 0.13 0.04 0.18 0.41 2.06 0.03 0.00 0.01 0.85 0.04 0.01
最大值 76.36 7.08 5.73 6.77 98.49 499.75 4.18 0.13 0.73 289.74 5.29 4.76
偏度 8.70 12.81 5.95 4.48 10.71 7.01 12.26 6.70 8.97 17.23 15.76 14.77
峰度 103.25 205.89 43.46 27.03 142.63 60.77 168.01 66.67 101.71 318.10 285.21 255.09
变异系数 1.11 1.07 1.98 1.08 1.70 2.65 2.22 0.86 1.28 4.80 1.38 2.52
Table 1  地电提取元素含量统计参数
Fig.5  元素含量对数转换后的箱状图
Fig.6  聚类分析树状图
元素 Ti V Co Ni Cu Zn As Mo Sb Pb Th U
Ti 1.000
V 0.840 1.000
Co 0.533 0.570 1.000
Ni 0.562 0.501 0.563 1.000
Cu 0.332 0.397 0.248 0.341 1.000
Zn 0.074 0.107 0.047 0.101 0.116 1.000
As 0.743 0.658 0.366 0.413 0.325 0.068 1.000
Mo 0.674 0.720 0.342 0.452 0.327 0.107 0.718 1.000
Sb 0.312 0.261 0.111 0.294 0.164 -0.002 0.664 0.590 1.000
Pb 0.542 0.356 0.183 0.234 0.183 0.039 0.904 0.469 0.661 1.000
Th 0.810 0.891 0.488 0.406 0.366 0.122 0.642 0.660 0.139 0.368 1.000
U 0.715 0.923 0.527 0.422 0.411 0.111 0.619 0.688 0.202 0.307 0.887 1.000
Table 2  因子分析的变量相关系数矩阵
元素 F1 F2 F3
Ti 0.740 - 0.363 0.371
V 0.894 - 0.193 0.318
Co 0.378 0.005 0.782 -
Ni 0.205 0.220 0.864 -
As 0.529 0.797 - 0.161
Mo 0.622 - 0.539 0.209
Sb -0.003 0.900 - 0.143
Pb 0.234 0.883 - 0.022
Th 0.935 - 0.140 0.185
U 0.911 - 0.132 0.231
方差贡献率/% 39.579 27.690 17.746
累计方差贡献率/% 39.579 67.268 85.015
Table 3  正交旋转因子载荷矩阵及因子方差贡献累计
元素 背景值 标准差 外带下限 中带下限 内带下限
Ti 3.576 1.367 4.942 6.309 9.043
V 0.302 0.081 0.383 0.464 0.627
Co 0.127 0.046 0.172 0.218 0.309
Ni 0.384 0.119 0.503 0.622 0.860
As 0.121 0.044 0.164 0.208 0.296
Mo 0.010 0.004 0.014 0.019 0.028
Sb 0.035 0.017 0.052 0.069 0.103
Pb 1.511 0.380 1.891 2.271 3.031
Th 0.169 0.063 0.232 0.295 0.422
U 0.060 0.024 0.084 0.108 0.156
Table 4  江西相山矿区各元素异常分带值
Fig.7  游坊地区地电提取单元素异常平面图及w(U)/w(Th)比值平面
1—新元古界;2—白垩系下统鹅湖岭组;3—白垩系下统打鼓顶组;4—次斑状花岗岩;5—地电测网;6—断裂构造;7—地质界线;8—异常内带;9—异常中带;10—异常外带;11—地名;12—AMT推测基底深度
Fig.8  游坊地区元素组合异常
1—新元古界;2—白垩系下统鹅湖岭组;3—白垩系下统打鼓顶组;4—次斑状花岗岩;5—地电测网;6—断裂构造;7—地质界线;8—异常内带;9—异常中带;10—异常外带;11—地名
Fig.9  地质—地电化学综合找矿模式
1—新元古界;2—白垩系下统鹅湖岭组;3—次斑状花岗岩;4—断裂构造; 5—地质界线;6—矿体;7—不整合接触
Fig.10  相山矿区靶区预测
1—新元古界;2—白垩系下统鹅湖岭组;3—白垩系下统打鼓顶组;4—次斑状花岗岩;5—地电测网;6—断裂构造;7—地质界线;8—AMT推测基底深度;9—2号靶区;10—1号靶区;11—地名
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