玲珑金矿大开头矿区47号脉微量元素特征

高海东; 胡宝群; 吕古贤; 武际春; 郭涛; 王志华; 王乃伟; 李元志

玲珑金矿大开头矿区47号脉微量元素特征

高海东^{1, 2,},
胡宝群¹,
吕古贤³,
武际春⁴,
郭涛²,
王志华⁵,
王乃伟⁴,
李元志¹

1.
东华理工大学地球科学学院, 江西抚州 344000
2.
江西省核工业地质调查院, 南昌 330000
3.
中国地质科学院地质力学研究所, 北京 100081
4.
山东黄金矿业(玲珑)有限公司, 山东招远 265419
5.
河南省地矿局第五地质勘查院, 郑州 450000

基金项目:

地质调查项目 1212011220935

国家自然科学基金项目 40862005

国家自然科学基金项目 40872165

详细信息

作者简介:
高海东(1983-), 男, 山西省大同市人, 硕士研究生, 地球化学专业。E-mail:yanhong04011230@126.com

中图分类号: P618.51
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出版历程
- 收稿日期: 2012-10-17
- 刊出日期: 2013-06-01

TRACE ELEMENT CHARACTERISTICS OF THE NO.47 VEIN IN DAKAITOU ORE DISTRICAT OF LINGLONG GOLD DEPOSIT

1.
School of Earth Science, East China Institute of Technology, Fuzhou 344000, Jiangxi, China
2.
Nuclear Industry Geological Bureau of Jiangxi Province, Nanchang 330000, China
3.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
4.
Shandong Gold Corporation Group Limited, Zhaoyuan 265419, Shandong, China
5.
The No.5 Institute of Geo-Exploration of Henan, Zhengzhou 450000, China

摘要

摘要: 选择胶东玲珑金矿典型矿体47号脉为研究对象，应用基岩地球化学方法，测试微量元素含量，研究微量元素与金的相关关系、计算微量元素的浓集系数并确定其轴向分带，探讨微量元素对深部金成矿的指示意义，期待能对玲珑金矿深部找矿提供一些参考。初步认识如下：矿区金矿体的最佳指示元素依次为Au、Ag、Bi、As、Cu、Co、Mo、Sb；金矿体的轴向分带序列从上到下依次为As、Pb、Ag、Cu、Hg、Sb、Mo、Ni、Th、V、U、Mn、Zn、Bi、Co、Au；矿体中Au、Bi、Ag、As富集系数大，Cu、Co富集系数中等，而Zn在矿体中相对亏损。研究结果表明，在深部47号矿体仍有较好的成矿前景。
- 基岩地球化学 /
- 微量元素特征 /
- 玲珑金矿47号脉
Abstract: After years of mining, the reserves of Jiaodong Linglong gold deposit have been consumed enormously. Therefore, the prospecting of reserve resources has become an urgent problem. In this paper, by using the application of rock geochemical method and choosing the typical ore 47 vein as the object of study, the trace elements related with Au had been tested and the correlation between trace elements and Au had been researched. Then, the concentration coefficient and axial zoning had been calculated and the indicative significance of trace elements to deep Au mineralization had been discussed. Finally, looking forward to some reference can be provided for the prospecting of Linglong gold deposit at depth. Some preliminary recognition as followed that the optimal indicator elements in gold ore body is Au, Ag, Bi, As, Cu, Co, Mo and Sb successively; the axial zonality sequence from top to bottom is As, Pb, Ag, Cu, Hg, Sb, Mo, Ni, Th, V, U, Mn, Zn, Bi, Co and Au; the enrichment coefficient of Au, Bi, Ag is big, Cu and Co is medium, Zn is of relative depletion; and the mineralization prospect of No.47 ore body is good in deep.
- rock geochemistry /
- characteristics of trace elements /
- the No.47 vein of Linglong gold deposit

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图 1 玲珑金矿田矿区地质略图与大开头矿区89线地质剖面图

Figure 1. Geological sketch map and No.89 geological profile of Da kai-tou of Linglong Au deposit

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图 2 含多条硅化硫化物线及细脉的矿体

Figure 2. The orebody with linear silicide and vulcanization vein

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图 3 硅化硫化物矿体

Figure 3. The orebody of silicide and vulcanization vein

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图 4 微量元素相关性对比图

（LL307、LL335、LL080、LL106、LL298等5个样品中Au含量远高于其他样品，使曲线变化规律不明显，已剔除）

Figure 4. The relevance of trace elements

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图 5 47号脉矿石及围岩基岩地球化学微量元素平均值对数曲线图

Figure 5. The relevance of average value of trace element in different rock about No.47 vein

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表 1 47号脉部分基岩地球化学元素成分

Table 1. Part of the rock geochemical elements contents of No.47 vein

表 2 47号脉矿石及围岩基岩地球化学微量元素平均值

Table 2. Average of all rock geochemical composition analysis of silicate of No.47 vein

表 3 背景样及背景值

Table 3. Background samples and background values of the deposit

表 4 47号脉基岩地球化学微量元素的浓集系数

Table 4. The concentration ratio about rock geochemical trace elements in the No.47 vein

表 5 47号脉基岩地球化学微量元素浓集程度

Table 5. Concentration ratio about rock geochemical trace elements in the No.47 vein

表 6 47号脉原生晕的线金属量

Table 6. The zoning about line metal content of the No.47 vein

表 7 浓集系数表

Table 7. The center of element enrichment of the No.47 vein

参考文献(7)

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