江西科学2011，Vol.29Issue(4)：506-509,4.
辽宁省连山关铀矿床绿泥石形成环境与铀矿化关系
The Formation Environment of Chlorite and Its＇ Relationship with Uranium Mineralization in Lianshanguan Uranium Deposit, Liaoning Province
摘要
Abstract
The paper adopts the technique of electron probe microanalysis, to study the alteration features, chemical composition and formation environment of chlorite in Lianshanguan uranium deposite ,and preliminary interpretates the formation environment of chlorite and its＇relationship with uranium mineralization. The paper indicates the chlorite formed at 242.54 - 286.89 ℃. The Ripidolite, Brunsvigite, Pycnochloriteg, Diabantite are detected during the studying. The mineralize solution deposited in the reducing environment. So the chlorite offers a favourable deposit environment.关键词
绿泥石/形成环境/铀矿化Key words
Chlorite/Formation environment/Uranium mineralization分类
天文与地球科学引用本文复制引用
章卫星,肖志伟,刘成东..辽宁省连山关铀矿床绿泥石形成环境与铀矿化关系[J].江西科学,2011,29(4):506-509,4.基金项目
浙江省地质勘查局基金项目 （）
