铀矿地质2011，Vol.27Issue(4)：215-220,256,7.
新疆白杨河铀铍矿床围岩蚀变及其地球化学特征
The wall rock alteration and its geochemical characteristics of Baiyanghe uranium and beryllium deposit, Xinjiang
修晓茜 1范洪海 2马汉峰 2衣龙升2
作者信息
- 1. 中国地质大学(北京)地球科学与资源学院，北京100083
- 2. 核工业北京地质研究院，中核铀资源勘查与评价技术重点实验室，北京100029
- 折叠
摘要
Abstract
This paper studied the alteration characteristics of near ore wall rocks in Baiyanghe uranium and beryllium deposit, Xinjiang. It was found that the main wallrock alteration is hematitization and fluo-ritization . Geochemical analysis result of rocks from the deposit suggested that near the central zone of mineralization, the content of silicate decreased while the concents of Ca and Mg increased, the content of Pb, Mo, Sb correlate positively with uranium content and therefore they can be used as the indicators for uranium exploration .关键词
铀铍矿床；蚀变特征；元素迁移富集；白杨河Key words
uranium and beryllium deposit/ alteration characteristics/ elemental migration/ Baiyanghe分类
天文与地球科学引用本文复制引用
修晓茜,范洪海,马汉峰,衣龙升..新疆白杨河铀铍矿床围岩蚀变及其地球化学特征[J].铀矿地质,2011,27(4):215-220,256,7.
