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物探与化探  2020, Vol. 44 Issue (1): 1-12    DOI: 10.11720/wtyht.2020.1060
     地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
安徽省祁门—黟县地区水系沉积物地球化学特征及找矿方向
翁望飞, 王德恩, 王邦民, 丁勇, 王拥军
安徽省地质矿产勘查局 332地质队,安徽 黄山 245000
Geochemical characteristics of stream sediments and prospecting direction in Qimen-Yixian area of Anhui Province
Wang-Fei WENG, De-En WANG, Bang-Min WANG, Yong DING, Yong-Jun WANG
No. 332 Geological Party, Bureau of Geology and Mineral Resources Exploration of Anhui Province, Huangshan 245000, China
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摘要 

在安徽祁门—黟县地区开展1∶50 000水系沉积物测量,采集样品5 386件,通过水系沉积物样品分析结果的数理统计,对成矿元素地球化学特征进行了研究。利用元素地球化学特征参数、R型聚类分析结果划分了高、中、低温3个元素组合类型,组合异常的分布规律反映了祁门—黟县地区多金属元素富集主要受燕山期岩浆—构造成矿体系和寒武系黑色岩系控制。在此基础上,结合地质、矿产分布特征,圈定了6处多金属矿成矿远景区,主攻矿种为金多金属矿,目标矿床类型为岩浆热液充填型、矽卡岩型。利用水系沉积物测量成果,在祁门黄古田、金家山等地开展异常查证与矿产勘查,发现了一批金、铅锌矿体,表明该方法在本地区具有良好的找矿应用价值。

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翁望飞
王德恩
王邦民
丁勇
王拥军
关键词 水系沉积物地球化学特征衬值异常找矿远景区祁门—黟县地区;    
Abstract

Based on 1∶50 000 stream sediments survey and mathematical statistics of analytical results of 5 386 samples, the authors conducted an in-depth study of the geochemical characteristics of ore-forming elements of Qimen-Yixian area in Anhui Province. Through element geochemical characteristics analysis and R cluster analysis, the element combination was divided into three types, namely, high temperature anomaly, medium temperature anomaly and low temperature anomaly. The distribution law of combined anomalies shows polymetallic element enrichment in Qimen-Yixian area, mainly controlled by Yanshanian magmatic-tectonic mineralization system and Cambrian black rock series. On such a basis, six polymetallic metallogenic prospective areas were delineated according to geological and mineral resources features. Gold was selected as the dominant mineral, and the target deposit types are magmatic hydrothermal filling and skarn types. Anomaly verification and mineral exploration were carried out in Huanggutian, Guxi, Jinjiashan areas of Qimen County based on the results of the stream sediments survey. A batch of gold, tungsten, molybdenum orebodies were discovered, indicating that there exists great application value of prospecting in this area.

Key wordsstream sediments    geochemical characteristics    contrast value anomaly    metallogenic prospective province    Qimen-Yixian area
收稿日期: 2019-01-24      出版日期: 2020-03-03
ZTFLH:  P595  
  P632+.3  
基金资助:安徽省公益性地质工作项目(2008-g-3);安徽省公益性地质工作项目(2010-g-11);安徽省地质勘查基金项目(2011-2-12-1);安徽省地质勘查基金项目(2011-2-12-2);安徽省地质勘查基金项目(2011-2-12-3);安徽省地质矿产勘查局地质勘查基金项目(DK2013-2-06)
作者简介: 翁望飞(1980-),男,硕士,高级工程师,主要从事地质调查与矿产勘查工作。Email: fiyan@163.com
引用本文:   
翁望飞, 王德恩, 王邦民, 丁勇, 王拥军. 安徽省祁门—黟县地区水系沉积物地球化学特征及找矿方向[J]. 物探与化探, 2020, 44(1): 1-12.
Wang-Fei WENG, De-En WANG, Bang-Min WANG, Yong DING, Yong-Jun WANG. Geochemical characteristics of stream sediments and prospecting direction in Qimen-Yixian area of Anhui Province. Geophysical and Geochemical Exploration, 2020, 44(1): 1-12.
链接本文:  
http://www.wutanyuhuatan.com/CN/10.11720/wtyht.2020.1060      或      http://www.wutanyuhuatan.com/CN/Y2020/V44/I1/1
Fig.1  祁门—黟县地区大地构造位置[8](a)及区域地质矿产简图(b)
1—新生界;2—侏罗系-白垩系陆相沉积盖层;3—南华系-三叠系海相沉积盖层;4—中-新元古界变质基底;5—燕山晚期花岗岩;6—燕山早-中期花岗岩;7—晋宁晚期花岗岩;8—晋宁早期花岗岩;9—蛇绿岩套(歙县伏川);10—主要断层;11—矿床点(黄色—金矿,绿色—铜矿;蓝色—铅锌矿;紫色—钨矿);12—研究区;F1—江南深断裂;F2—城安-镇头断裂;F3—祁门-三阳断裂;F4—祁门-五城断裂;F5—五城-绩溪断裂;F6—江湾-街口断裂
Fig.2  安徽省祁门—黟县地区地质矿产简图[9]
1—侏罗系-白垩系陆相盖层;2—南华系-寒武系海相盖层;3—青白口系浅变质碎屑岩;4—中-新元古界浅变质碎屑岩;5—侏罗纪花岗闪长斑岩;6—青白口纪黑云母花岗闪长岩;7—花岗斑岩脉;8—石英闪长玢岩脉;9—辉绿岩脉;10—辉长辉绿岩;11—断层及编号;12—脆韧性剪切带及编号;13—矿床(点);F1—城安-镇头逆冲挤压断裂带;F2—祁门-三阳断裂带;F3—社景-青岭山-古竹林韧性剪切带;F4—箬坑断裂;F5—铺岭断裂;F6—东源-历口断裂;F7—官田-六都断裂;F8—青岭山断裂;F9—渔亭断裂;F10—仙寓山断裂;F11—东源-柏溪断裂;(1)—祁门箬坑铜铅锌多金属矿点;(2)—祁门湘东铜矿点;(3)—祁门北坑铜矿化点;(4)—祁门东源钨钼矿(大型);(5)—祁门黄古田金矿;(6)—祁门廖家金矿(小型);(7)—祁门金家山金矿(小型);(8)—祁门汪家坦金矿点;(9)—祁门桃丰山锑矿;(10)—祁门三宝铅锌矿(中型);(11)—黟县官路下钨矿点;(12)—黟县屏山铅锌矿点;(13)—黟县石山钒矿(中型)
元素 分析方法 方法检出限/10-6
Au 石墨炉原子吸收 0.00005
W 示波极谱 0.2
Mo 示波极谱 0.26
Hg 发射光谱 0.0015
Ag 发射光谱 0.015
Pb 发射光谱 1.1
Zn 原子吸收 4
Cu 原子吸收 0.4
Sb 原子荧光 0.042
Bi 原子荧光 0.02
As 原子荧光 0.24
Table 1  水系沉积物样品分析方法及检出限
参数 Sb Pb As Bi Cu Ag Zn Hg Mo W Au
平均值(Xˉ) 1.77 32.44 14.36 0.86 29.03 115.81 122.36 136.08 1.65 3.82 2.73
最大值(Xmax) 100 1000 295.10 100 400 10000 501.2 10665 93.88 263.74 291.89
标准离差(S) 2.83 22.98 15.50 2.59 20.67 301.17 44.26 284.35 4.06 7.80 8.60
变异系数(Cv) 1.60 0.71 1.08 3.00 0.71 2.60 0.36 2.09 2.46 2.04 3.15
背景值 1.24 30.99 11.05 0.63 26.35 83.68 119.52 102.83 0.86 2.83 1.81
浓集系数(K) 2.17 1.21 1.37 2.24 1.14 0.92 1.64 2.11 1.32 1.35 1.08
Table 2  祁门—黟县地区水系沉积物地球化学特征参数
Fig.3  祁门—黟县地区成矿元素变异系数离散程度图解
Cv1—循环剔除高低值前变异系数;Cv2—循环剔除高低值后变异系数
元素 参数 地层单元
Pt2-3 Nh-∈ J-K γ
Xˉ 2.61 2.61 3.11 3.89
Au S 8.57 3.04 13.24 9.83
Cv 3.29 1.17 4.26 2.53
Xˉ 91.02 416.68 156.71 91.28
Ag S 97.79 905.94 792.24 61.35
Cv 1.07 2.17 5.06 0.67
Xˉ 29.76 37.15 17.96 19.41
Cu S 19.71 29.75 11.08 18.20
Cv 0.66 0.80 0.62 0.94
Xˉ 32.55 43.19 24.43 25.35
Pb S 12.25 73.38 8.98 11.78
Cv 0.38 1.70 0.37 0.47
Xˉ 125.49 146.24 77.97 88.73
Zn S 36.31 84.46 35.08 41.15
Cv 0.29 0.58 0.45 0.46
Xˉ 3.24 4.08 3.94 9.08
W S 5.94 4.36 3.30 17.90
Cv 1.84 1.07 0.84 1.97
Xˉ 126.01 216.11 302.29 110.04
Hg S 193.82 378.44 1135.94 130.78
Cv 1.54 1.75 3.76 1.19
Xˉ 0.97 8.13 1.24 2.91
Mo S 1.12 10.14 0.93 7.45
Cv 1.15 1.25 0.75 2.56
Xˉ 0.69 1.20 0.52 2.34
Bi S 1.60 2.54 0.30 6.74
Cv 2.32 2.12 0.59 2.88
Xˉ 13.84 24.75 25.42 7.15
As S 12.91 31.03 22.41 8.78
Cv 0.93 1.25 0.88 1.23
Xˉ 1.69 3.17 2.85 0.97
Sb S 2.55 5.24 4.03 0.92
Cv 1.51 1.65 1.42 0.95
Table 3  不同地质单元水系沉积物地球化学特征参数
Fig.4  祁门—黟县地区水系沉积物成矿元素聚类分析谱系
Fig.5  祁门—黟县地区水系沉积物主成矿元素异常及找矿远景区
Fig.6  祁门金家山西坑金矿点地质简图
1—元古宇牛屋组下段;2—元古宇环沙组;3—特殊岩性层:紫红色泥质粉砂岩;4—花岗斑岩脉;5—石英脉;6—石英闪长玢岩脉;7—安山玢岩脉;8—断裂构造带;9—土壤化探查证金异常;10—土壤化探查证砷异常;11—板理产状;12—探槽查证位置及编号;13—金矿体;14—河流及流向
Fig.7  祁门地区金矿石照片
a—金家山毒砂矿化蚀变岩型金矿石(TC25);b—黄古田细脉状毒砂矿化石英脉型金矿石(TC6);c—黄古田毒砂矿化构造蚀变岩型金矿石
Fig.8  祁门黄古田金矿点地质简图
1—元古宇牛屋组下段;2—元古宇牛屋组上段;3—元古宇环沙组;4—煌斑岩脉;5—石英脉;6—断裂;7—地层界线;8—探槽;9—金矿体;10—产状;11—土壤化探金异常和砷异常及其下限;12—河流及流向
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