Quantitative prediction of mineral resources in typical gold deposits in Guangxi, China using a fuzzy weights of evidence method
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摘要: 多信息融合的矿产资源定量预测是当前资源潜力预测的前缘课题,不同地质背景信息与地球化学数据的深度挖掘是当前该领域急需解决的关键问题。文章通过总结广西各构造单元地质背景和成矿控制要素,在ArcGIS、GeoDAS等软件平台基础上,分析了广西全区60767个地球化学样品中Au、Ag、Mn、Cu、Pb、Zn、Sn、Sb等主要成矿及伴生元素的空间分布特征。基于GeoDAS平台,通过IDW插值、S-A异常分解、主成分分析等技术,选取地球化学组合元素异常、重磁异常以及岩浆岩与断层交点缓冲区数据,通过模糊证据权模型,重点选取卡林型金矿和破碎带蚀变金矿2种典型矿产类型,编制了成矿后验概率图,圈定了金成矿有利地段。该研究对应用新的成矿理论和评价技术方法在广西开展矿产资源潜力评价以及区划工作具有重要的参考意义。Abstract: Quantitative prediction of mineral resources based on multi-information fusion is the leading topic of resource potential prediction, in which the deep mining of different geological background information and geochemical data is the key problem and still challenging. In this study, we analyzed the spatial distribution characteristics of main metallogenic and associated elements such as Au, Ag, Mn, Cu, Pb, Zn, Sn and Sb in 60767 geochemical samples on the platforms like ArcGIS and GeoDAS, by summerzing the geological background information and metallogenic controlling factors of each tectonic unit in Guangxi. Based on the GeoDAS paltform, through IDW interpolation, S-A anomaly decomposition, principal component analysis and other technologies, the data from the layers with geochemical component element anomaly, gravity and aeromagnetic anomaly and the buffers at the intersection of magmatic rock and fault were used as the training points for the utilization of the fuzzy weights of evidence. A posteriori probability map was drawn up to delineate the favorable metallogenic areas for Carlin-type gold deposit and fracture zone altered gold deposit. This study is of great significance to the application of new metallogenic theories and evaluation techniques in the evaluation or zoning of mineral resources potential.
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图 10 布格重力异常图层隶属度函数v-t图解及模糊证据权重的选择示意图(红色点表示与成矿密切相关的点、蓝色点表示与成矿关系不密切的点)
Figure 10. V-T diagram of membership function of Bouguer gravity anomaly layer and selection of fuzzy evidence weights (red points indicate points closely related to mineralization, blue points indicate points not closely related to mineralization)
图 11 采用模糊证据权法计算的金的后验概率图及资源潜力远景区预测
I-桂中加里东地槽褶皱带(I1-桂北隆起;I2-柳州坳陷;I3-桂东北过渡带;I4-大瑶山隆起;I5-云开隆起);II-桂南海西地槽褶皱带;III-桂西印支地槽褶皱(III1-都阳山隆起III2-右江坳陷;III3-西大明山隆起;III4-十万大山坳陷);1-四堡断裂2-平珮岭断裂;3-三江-融安断裂;4-寿城断裂;5-龙胜-永福断裂;6-资源断裂;7-陆川-岑溪断裂;8-博白-梧州断裂;9-灵山-藤县断裂;10-峒中-小董断裂带;11-高屏-新黑断裂;12-凭祥-大黎断裂带;13-荔浦断裂;14-下雷-灵马断裂;15-那坡断裂带;16-右江断裂带;17-田林-巴马断裂带;18-南丹-昆仑关断裂带;19-白石断裂;20-栗木-马江断裂;21-富川断裂;22-桂林-来宾断裂带;23-观音阁断裂带;24-宜山-柳城断裂带a-依据PCA1背景与异常分解后卡林型金矿预测后验概率图; b-依据PCA3背景与异常分解后破碎带蚀变型金矿预测后验概率图
Figure 11. Posterior probability map of Au and target areas for gold deposits delineated by the fuzzy weights of evidence method. (a) Carlin-type gold deposits predicted by PCA1 background and anomaly decomposition. (b) Altered type gold deposits predicted by PCA3 background and anomaly decomposition I-Caledonian geosynclinal fold belt in Central Guangxi (I1-Northern Guangxi uplift; I2-Liuzhou depression; I3-Northeast Guangxi transitional zone; I4-Dayaoshan uplift; I5-Yunkai uplift); II-Hercynian geosynclinal fold belt in southern Guangxi; III-Indosinian geosynclinal fold in Western Guangxi (III1-Duyangshan uplift; III2-Youjiang depression; III3-Xidamingshan uplift; III4-Shiwandashan depression); 1-Sipu fault, 2-Pingpeiling fault; 3-Sanjiang-rong′an fault; 4-Shoucheng fault; 5-Longsheng-Yongfu fault; 6-Ziyuan fault; 7-Luchuan-Cenxi fault; 8-Bobai-Wuzhou fault; 9-Lingshan-Tengxian fault; 10-Dongzhong-Xiaodong fault zone; 11-Gaoping-Xinhei fault; 12-Pingxiang-Dali fault zone; 13-Lipu fault; 14-Xialei-Lingma fault; 15-Napo fault zone; 16-Youjiang fault zone; 17-Tianlin-Bama fault zone; 18-Nandan-Kunlunguan fault zone; 19-Baishi fault; 20-Limu-Majiang fault; 21-Fuchuan fault; 22-Guilin-Laibin fault zone; 23-Guanyin′ge fault zone; 24-Yishan-Liucheng fault zone
图 13 卡林型金矿预测靶区与广西有色金属成矿带分布
I-丹池锡-铜-铅-锌-银-锑-汞成矿带;II-桂北锡-钨-铜-镍-铅-锌成矿带;III-桂东北锡-钨-铜-铅-锌-金-银成矿带;IV-大明山钨-铜-金成矿带;V-大瑶山铜-铅-锌-金成矿带;VI-云开大山铅-锌-钨-金成矿带;VII-西大明山铜-铅-锌-银成矿带;VIII-桂西金-锑成矿带;IX-靖西-平果铝成矿带
Figure 13. Distribution of Carlin-type gold deposits predicted target area and Guangxi nonferrous metal metallogenic belts I-Danchi metallogenic belt of Sn-Cu-Pb-Zn-Ag-Sb-Hg; II-Northern Guangxi metallogenic belt of Sn-W-Cu-Ni-Pb-Zn; III-Northeastern Guangxi metallogenic belt of Sn-W-Cu-Pb-Zn-Au-Ag; IV-Damingshan metallogenic belt of W-Cu-Au; V-Dayaoshan metallogenic belt of Cu-Pb-Zn-Au; VI-Yunkaidashan metallogenic belt of Pb-Zn-W-Au; VII-West Damingshan metallogenic belt of Cu-Pb-Zn-Ag; VIII-Western Guangxi metallogenic belt of Au-Sb; IX-Jingxi-Pingguo metallogenic belt of Al
图 14 证据权法破碎带蚀变岩型金矿预测与广西有色金属成矿带分布图
I-丹池锡-铜-铅-锌-银-锑-汞成矿带;II-桂北锡-钨-铜-镍-铅-锌成矿带;III-桂东北锡-钨-铜-铅-锌-金-银成矿带;IV-大明山钨-铜-金成矿带;V-大瑶山铜-铅-锌-金成矿带;VI-云开大山铅-锌-钨-金成矿带;VII-西大明山铜-铅-锌-银成矿带;VIII-桂西金-锑成矿带;IX-靖西-平果铝成矿带
Figure 14. Prediction map of altered rock type gold deposits in fracture zone by the weights of evidence method and the distribution of Guangxi nonferrous metal metallogenic belts I-Danchi metallogenic belt of Sn-Cu-Pb-Zn-Ag-Sb-Hg; II-Northern Guangxi metallogenic belt of Sn-W-Cu-Ni-Pb-Zn; III-Northeastern Guangxi metallogenic belt of Sn-W-Cu-Pb-Zn-Au-Ag; IV-Damingshan metallogenic belt of W-Cu-Au; V-Dayaoshan metallogenic belt of Cu-Pb-Zn-Au; VI-Yunkaidashan metallogenic belt of Pb-Zn-W-Au; VII-West Damingshan metallogenic belt of Cu-Pb-Zn-Ag; VIII-Western Guangxi metallogenic belt of Au-Sb; IX-Jingxi-Pingguo metallogenic belt of Al
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