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云南剑川老君山新生代盆地铀矿化特征

李文贤

铀矿地质Issue(5):276-282,7.
铀矿地质Issue(5):276-282,7.DOI:10.3969/j.issn.10000658.2014.05.004

云南剑川老君山新生代盆地铀矿化特征

Uranium Mineralization Characteristics of Cenozoic Jianchuan Laoj unshan Basin in Yunnan

李文贤1

作者信息

  • 1. 核工业 280 研究所,四川 广汉 618300
  • 折叠

摘要

Abstract

Jianchuan Laojunshan Cenozoic basin is an inheritance one which lies on the basement of Tri-assic Shizhongshan group and is covered by Neogene Jianchuan group.Jianchuan group is a set of volcanic sedimentary rocks composed by trachyte, tuff, volcanic breccia, agglomerate and lava, tuffaceous sandstone,lithic sandstone.Uranium mineralization was found in six types rocks,Tuff,sandstone,sy-enite porphyry,granite porphyry,trachyte and granitic pegmatite in the basin.Studies shew that Jian-chuan basin is with good exploration potential.Due to the combined effects of regional faults,volcanic activity and volcanic structure.

关键词

铀矿化特征/新生代盆地/剑川/老君山

Key words

characteristics of uranium mineralization/Cenozoic basins/Jianchuan Laojunshan

分类

天文与地球科学

引用本文复制引用

李文贤..云南剑川老君山新生代盆地铀矿化特征[J].铀矿地质,2014,(5):276-282,7.

铀矿地质

OACSCD

1000-0658

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