华南与花岗岩有关的稀有金属矿床和钨锡矿床的时空分布规律及其成因联系

吴堑虹; 周厚祥; 刘飚; 孔华; 裴进云; 覃毅学; 宗琦; 吴锟言; 汤钰御

doi:10.19509/j.cnki.dzkq.2022.0047

华南与花岗岩有关的稀有金属矿床和钨锡矿床的时空分布规律及其成因联系

doi: 10.19509/j.cnki.dzkq.2022.0047

吴堑虹^{1a, 1b,},
周厚祥^{2, 3},
刘飚^{1a, 1b, ,},
孔华^{1a, 1b},
裴进云⁴,
覃毅学^{1a, 1b},
宗琦^{1a, 1b},
吴锟言^{1a, 1b},
汤钰御^{1a, 1b}

1a.
中南大学地球科学与信息物理学院, 长沙 410083
1b.
中南大学有色金属成矿预测与地质环境监测教育部重点实验室, 长沙 410083
2.
湖南省自然资源事务中心, 长沙 410004
3.
洞庭湖区生态环境遥感监测湖南省重点实验室, 长沙 410004
4.
中国冶金地质总局第三地质勘查院, 太原 030002

基金项目:

国家重点研发计划 2018YFC0603902

湖南省自然资源厅项目 20190604

湖南省自然科学青年基金项目 2021JJ40722

详细信息

作者简介:
吴堑虹(1957— ), 教授, 主要从事区域成矿规律研究工作。E-mail: qhwu@csu.edu.cn

通讯作者:
刘飚(1989— ), 讲师, 主要从事矿床学方面研究工作。E-mail: biaoliu@csu.edu.cn

中图分类号: P618.4
计量
- 文章访问数: 1901
- PDF下载量: 223
- 被引次数: 0
出版历程
- 收稿日期: 2021-06-02

Spatio-temporal distribution of granite-related rare metal deposits and W-Sn deposits in South China and their genetic relationship

Wu Qianhong^{1a, 1b
,},
Zhou Houxiang^{2, 3},
Liu Biao^{1a, 1b
, ,},
Kong Hua^{1a, 1b},
Pei Jinyun⁴,
Qin Yixue^{1a, 1b},
Zong Qi^{1a, 1b},
Wu Kunyan^{1a, 1b},
Tang Yuyu^{1a, 1b}

1a.
School of Geoscience and InfoPhysics, Central South University, Changsha 410083, China
1b.
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083, China
2.
Hunan Natural Resources Affairs Center, Changsha 410004, China
3.
Hunan Key Laboratory of Remote Sensing Monitoring of Ecological Environment in Dongting Lake Area, Changsha 410004, China
4.
The No.3 Bureau of China Metallurgical Geology Bureau, Taiyuan 030002, China

摘要

摘要:
华南是我国战略性矿产钨锡的主产地，且与花岗岩有关的钨锡矿床附近常发育Li、Rb、Be、Nb、Ta等稀有金属矿床，但对这两类矿床的成因联系并不清楚。通过收集整理华南与花岗岩有关的稀有金属矿床和钨锡矿床的研究资料，对稀有金属矿和钨锡矿的成因关系进行初步分析，认识到这两类矿床具有区域-矿田-矿床-矿物多尺度的空间相关性，成矿时代、成矿物质来源及成矿作用相近性，且成矿主要与燕山期高分异花岗岩有关。两者之间“偶极”式分布样式为利用华南极为丰富的钨锡矿床勘探及研究成果寻找稀有金属矿床提供了依据。
- 与花岗岩有关 /
- 稀有金属矿 /
- 钨锡矿床 /
- 成因关系 /
- 时空分布 /
- 华南
Abstract:
The strategic mineral W-Sn deposits in China are mainly concentrated in South China, and many rare metal mineralizations, such as Li, Rb, Be, Nb, Ta, etc., are often coproduced with them. However, the genetic relationship between them is unclear. Based on the analysis of research data related to granite-related rare metals and W-Sn deposits in South China, we believe that the two types of mineralization have a close spatio-temporal relationship at multiple scales, such as metallogenic belts, ore fields, deposits, and minerals. In addition, the ore-forming material source, mineralization process, and ore-controlling structures are similar, indicating that they may have derived from a same granitic mass and the mineralization usually have close genetic relationship with the high evolved granite. Therefore, the exploration and research data of W-Sn deposits in South China can be used to explore and study rare metal deposits.
- granite related /
- rare metal deposit /
- W-Sn deposit /
- genetic relationship /
- spatio-temporal distribution /
- South China

HTML全文

图 1 典型矿床稀有金属矿-钨锡矿相对位置示意图

a.湖南香花岭地区^[5]；b.江西大湖塘矿集区^[6]；c.湖南邓阜仙地区^[7]

Figure 1. Schematic diagram of the relative position of rare metal ore tungsten tin ore in a typical deposit

下载: 全尺寸图片幻灯片

图 2 大吉山矿田中稀有金属矿与钨锡矿分布示意图^[14]

Figure 2. Schematic diagram of the relative position of rare metals and W-Sn deposits in a typical ore field

下载: 全尺寸图片幻灯片

图 3 铌钽矿物与钨、锡矿物中相应元素分布图^{[6, 16, 18]}

Figure 3. Distribution diagram of elements in Nb-Ta and W-Sn minerals

下载: 全尺寸图片幻灯片

图 4 华南地区含稀有金属与钨锡花岗岩岩石化学特征变化

Figure 4. Petrochemical changes in rare metal and W-Sn granites in South China

下载: 全尺寸图片幻灯片

图 5 华南地区稀有金属与钨锡矿床综合成矿模式

Figure 5. Metallogenic model of rare metal and W-Sn deposits in South China

下载: 全尺寸图片幻灯片

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