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粤北希望铀矿床深部及其西部外围找矿前景

刘文泉 吴烈勤 李俊

铀矿地质Issue(4):426-431,6.
铀矿地质Issue(4):426-431,6.DOI:10.3969/j.issn.10000658.2015.04.002

粤北希望铀矿床深部及其西部外围找矿前景

Discussion on Prospecting Potential in the Depth and Western Periphery of Xiwang Uranium Deposit,Northern Guangdong

刘文泉 1吴烈勤 2李俊3

作者信息

  • 1. 东华理工大学,江西南昌330013
  • 2. 核工业290研究所,广东韶关512029
  • 3. 核工业290研究所,广东韶关512029
  • 折叠

摘要

Abstract

Based on the study of geological setting and ore controlling factor for uranium metallization and the exploration results in these years at the west of Xiwang uranium deposit ,we conclude that urani‐um deposit was formed in place where structures , magma and hydrothermal alteration over‐lapped.Uranium mineralization is strongly controlled by NNE ,NEE trending silicified fracture zones , uranium mineralization was strictly controlled by the silicified cataclastic rock near the fracture zones and the contact surface between granites of different phases. There is a highly prospecting potential and developing foreground at the intersection point of Xinqiao fault and the upper wall of NNE ,NEE trending silicification zone.

关键词

控矿因素/找矿前景/希望铀矿床/硅化断裂带

Key words

ore controlling factor/prospecting foreground/Xiwang uranium deposit/silicified fracture zone

分类

天文与地球科学

引用本文复制引用

刘文泉,吴烈勤,李俊..粤北希望铀矿床深部及其西部外围找矿前景[J].铀矿地质,2015,(4):426-431,6.

基金项目

中央地质勘查基金项目(编号2007441003)和中国核工业地质局铀矿地质项目(编号200722)共同资助。 ()

铀矿地质

OACSCD

1000-0658

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