Study of Mineral Mineral Composition and Occurrence State of Uranium in Pingshang Uranium Deposit

吴川福; 刘成东; 梁良; 刘洋; 谭双

doi:10.16056/j.1005-7676.2017.03.010

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Study of Mineral Mineral Composition and Occurrence State of Uranium in Pingshang Uranium Deposit

更新时间：2026-01-19

- Study of Mineral Mineral Composition and Occurrence State of Uranium in Pingshang Uranium Deposit
- Issue 3, Pages: 37-40(2017)
- 作者机构：
  
  东华理工大学省部共建核资源与环境国家重点实验室培育基地
- 作者简介：
- 基金信息：
- DOI：10.16056/j.1005-7676.2017.03.010
  CLC： P619.14
- Published：2017
- 稿件说明：
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[1]吴川福,刘成东,梁良,刘洋,谭双.江西坪上铀矿床矿石矿物组成及铀的赋存状态研究[J].能源研究与管理,2017(03):37-40.

吴川福, 刘成东, 梁良, et al. Study of Mineral Mineral Composition and Occurrence State of Uranium in Pingshang Uranium Deposit[J]. 2017, (3): 37-40.
[1]吴川福,刘成东,梁良,刘洋,谭双.江西坪上铀矿床矿石矿物组成及铀的赋存状态研究[J].能源研究与管理,2017(03):37-40. DOI： 10.16056/j.1005-7676.2017.03.010.

吴川福, 刘成东, 梁良, et al. Study of Mineral Mineral Composition and Occurrence State of Uranium in Pingshang Uranium Deposit[J]. 2017, (3): 37-40. DOI： 10.16056/j.1005-7676.2017.03.010.

摘要

坪上铀矿床位于桃山铀矿田内。通过野外现场取样后对样品进行镜下显微镜鉴定、人工重砂分析和电子探针分析等实验

基本查明:矿石中矿石矿物为沥青铀矿、铀石和钛铀矿;脉石矿物为长石、石英、云母、绿泥石和黄铁矿等;铀主要以独立铀矿物的形式存在

生长在长石和绿泥石等边缘。

Abstract

Ping uranium deposit is located in Taoshan uranium ore field.In this paper

the samples were sampled by microscopic microscopy

artificial heavy sand analysis and electron probe analysis.The ore minerals were asphalt

uranium and uranium

and the gangue minerals were long Stone

quartz

mica

chlorite and pyrite;uranium mainly in the form of independent uranium minerals exist in the growth of feldspar and chlorite and other edges.

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