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物探与化探  2023, Vol. 47 Issue (6): 1635-1642    DOI: 10.11720/wtyht.2023.0294
  稀有金属矿综合地气测量专栏 本期目录 | 过刊浏览 | 高级检索 |
青海茶卡北山锂铍矿勘查区X射线荧光异常特征及找矿意义
王亚栋1, 周四春2(), 刘晓辉2, 胡波2, 王广西2, 徐云甫1, 曹红亮1, 樊新胜2, 韩若浦2
1.青海省地质调查院 青藏高原北部地质过程与矿产资源重点实验室,青海 西宁 810012
2.成都理工大学 地学核技术四川省重点实验室,四川 成都 610059
X-ray fluorescence anomalies in the Chakabeishan exploration area for lithium-beryllium deposits, Qinghai Province:Characteristics and implications for prospecting
WANG Ya-Dong1, ZHOU Si-Chun2(), LIU Xiao-Hui2, HU Bo2, WANG Guang-Xi2, XU Yun-Fu1, CAO Hong-Liang1, FAN Xin-Sheng2, HAN Ruo-Pu2
1. Key Laboratory of the Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources, Qinghai Geological Survey Institute, Xining 810012, China
2. Applied Nuclear Technology in Geosciences Key Laboratory of Sichuan Province, Chengdu University of Technology, Chengdu 610059, China
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摘要 

在青海省乌兰县茶卡北山勘查区开展了土壤X射线荧光测量勘查伟晶岩锂铍矿的研究,结果表明,通过测量Ca、Ni、Mn、Fe以及Nb、Ta、Rb、K两组指示元素,可以准确捕获花岗伟晶岩锂铍矿形成的土壤次生晕。其中,第一组元素的X射线荧光异常信息用于指示含矿层位花岗伟晶岩的位置,第二组元素的X射线荧光异常则用于圈定具有矿化显示的伟晶岩脉的位置、走向及其在平面上的延伸范围。根据捕获的X射线荧光异常推测,勘查区主矿脉沿西北、东南两个方向还有较大延伸,该结论为下一步找矿工作提供了参考。

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王亚栋
周四春
刘晓辉
胡波
王广西
徐云甫
曹红亮
樊新胜
韩若浦
关键词 手提式X荧光仪土壤X射线荧光测量茶卡北山花岗伟晶岩锂铍矿    
Abstract

The research on exploring pegmatite-type lithium-beryllium deposits through soil X-ray fluorescence measurements was conducted in the Chakabeishan exploration area of Ulan County, Qinghai Province. The results demonstrate that soil secondary halos formed by granite pegmatite-type lithium-beryllium deposits can be accurately captured by measuring two groups of indicator elements, i.e., Ca, Ni, Mn, Fe, and Nb, Ta, Rb, K. The X-ray fluorescence anomalies of the first group of elements indicate the position of the ore-hosting horizon (i.e., granitic pegmatites). Those of the second group of elements are used to determine the location, strike, and planar extension range of the pegmatite veins with mineralization manifestation. As inferred from the captured X-ray fluorescence anomalies, the main ore veins in the exploration area exhibit significant extensions along the northwest and southeast directions. This conclusion provides a reference for further prospecting work.

Key wordshandheld X-ray fluorescence instrument    soil X-ray fluorescence measurement    Chaka North Mountain    granite pegmatite-type lithium-beryllium deposit
收稿日期: 2023-07-05      修回日期: 2023-10-07      出版日期: 2023-12-20
:  P632  
基金资助:青海省基础研究计划项目(2022-ZJ-751);国家重点研发计划项目(2017YFC0602701)
通讯作者: 周四春(1954-),男,成都理工大学教授,主要从事深部找矿技术方法研究及核技术应用。Email:zsc@cdut.edu.cn
作者简介: 王亚栋(1986-),男,物化探工程师,从事物化探勘查找矿工作。
引用本文:   
王亚栋, 周四春, 刘晓辉, 胡波, 王广西, 徐云甫, 曹红亮, 樊新胜, 韩若浦. 青海茶卡北山锂铍矿勘查区X射线荧光异常特征及找矿意义[J]. 物探与化探, 2023, 47(6): 1635-1642.
WANG Ya-Dong, ZHOU Si-Chun, LIU Xiao-Hui, HU Bo, WANG Guang-Xi, XU Yun-Fu, CAO Hong-Liang, FAN Xin-Sheng, HAN Ruo-Pu. X-ray fluorescence anomalies in the Chakabeishan exploration area for lithium-beryllium deposits, Qinghai Province:Characteristics and implications for prospecting. Geophysical and Geochemical Exploration, 2023, 47(6): 1635-1642.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2023.0294      或      https://www.wutanyuhuatan.com/CN/Y2023/V47/I6/1635
Fig.1  勘查区大地构造及交通位置(据王秉璋等[1]修改)
Fig.2  茶卡北山地区地质简图
1—实测地质界线;2—实测断层;3—伟晶岩脉;4—X射线荧光测线及编号;5—伟晶岩矿脉带;Qb-O3c—茶卡北山片岩组;C-P2g—石炭-二叠系果可山组;δoO3—奥陶系石英闪长岩;C-P2t—石炭—二叠系土尔根大坂组;Qhpal—全新统冲积物
Fig.3  XP3测线X射线荧光测量14种元素综合剖面
1—电气石花岗伟晶岩;2—石英闪长岩;3—二云母石英片岩;4—断层; 5—铍矿体;6—铍矿化体;7—钻孔及其编号;8—X射线荧光实测曲线
Fig.4  茶卡北山土壤X射线荧光测量Nb异常分布
Fig.5  茶卡北山X射线荧光测区东南端Nb异常(a)及推断解释(b)
1—地质界线; 2—断层; 3—实测土壤X射线荧光剖面; 4—X荧光异常带编号; 5—伟晶岩矿脉带; 6—推断伟晶岩脉;(a)中图例同图4;(b)中图例同图2
Fig.6  茶卡北山X射线荧光测区西北端Nb异常(a)及推断解释(b)(图例同图5)
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