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电子探针化学测年在攀枝花大田晶质铀矿中的应用及其意义

徐争启 欧阳鑫东 张成江 姚建 汤曼

岩矿测试2017,Vol.36Issue(6):641-648,8.
岩矿测试2017,Vol.36Issue(6):641-648,8.DOI:10.15898/j.cnki.11-2131/td.201704280071

电子探针化学测年在攀枝花大田晶质铀矿中的应用及其意义

Application of Electron Microprobe Chemical Dating to Datian Uraninite in Panzhihua and Its Significance

徐争启 1欧阳鑫东 1张成江 1姚建 2汤曼3

作者信息

  • 1. 成都理工大学地球科学学院,四川 成都 610059
  • 2. 核工业 280 研究所,四川 广汉 618300
  • 3. 四川省地质矿产勘查开发局 106 地质队,四川 温江 611130
  • 折叠

摘要

Abstract

As the main industrial uranium minerals in hydrothermal uranium deposits, uraninite and pitchblende are of great significance in the study of ore genesis and metallogenic regularity of hydrothermal uranium deposits.The Datian area in Panzhihua is one of the important areas of migmatite type hydrothermal uranium deposit in China.There is ultra-rich-uranium ore (U >10%) in rolling stone and the richer uranium-rich bedrock ore (U =0.1% -2%)where uraninite is the main uranium mineral.The study of the composition and forming age of two types of uraninite has important significance for metallogenic regularity of mixed rock type hydrothermal uranium deposits in the Datian area.In this study,mineralogical and Electron Microprobe analyses of uraninite in rolling stone and bedrock from the Datian area were carried out to determine the composition and age.Results show that the chemical compositions of uraninite in rolling stone and bedrock are similar except Pb contents with UO2 contents of 77.36% -84.04%, ThO2 contents of 0.98% -5.59%,and PbO contents of 1.79% -8.8%.Lead contents of uraninite in rolling stone are lower than those of uraninite in the bedrock,but thorium contents are contrary.Electron Microprobe chemical dating indicates that the uraninite in bedrock ore has ages of 774.9 -785.5 Ma,whereas the uraninite in rolling stones has an age of 783.7 Ma.The dating results are consistent with traditional isotopic dating (775 -777.6 Ma). The indicates that the uraninite in rolling stones and bedrock formed at the same time and the electronic probe in situ dating method is credible.In the late hydrothermal alteration,the uraninite experienced silicification, carbonization,and hematitization at 730.6 Ma,699.8 Ma,and 664.0 Ma,respectively.This study provides evidences for the metallogenic epoch and mineralization process of the hydrothermal uranium deposits.

关键词

晶质铀矿/电子探针定年/混合岩型铀矿/成矿时代/大田

Key words

uraninite/Electron Microprobe dating/migmatite type uranium deposits/metallogenic epoch/Datian

分类

天文与地球科学

引用本文复制引用

徐争启,欧阳鑫东,张成江,姚建,汤曼..电子探针化学测年在攀枝花大田晶质铀矿中的应用及其意义[J].岩矿测试,2017,36(6):641-648,8.

基金项目

中国核工业地质局科研项目(201637,201638) (201637,201638)

岩矿测试

OA北大核心CSCDCSTPCD

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