首页 | 本学科首页   官方微博 | 高级检索  
     

平邑卓家庄金矿床成矿地质特征
引用本文:祝德平,于超,廉永,杨忠臣,齐可昆. 平邑卓家庄金矿床成矿地质特征[J]. 黄金, 2001, 22(8): 11-14
作者姓名:祝德平  于超  廉永  杨忠臣  齐可昆
作者单位:山东省平邑归来庄金矿
摘    要:卓家庄金矿床是一个与中生代次火山杂岩体(二工闪长玢岩、二长斑岩)有关的小型金矿床,柱状矿体严格地受隐爆角砾岩筒的控制。从角砾岩筒中心向外,角砾粒度、成分、胶结物成分及蚀变均存在分带现象。全文着重阐述了金矿床地质特征,总结出矿床成矿规律,并对矿区成矿远景作了预测。

关 键 词:次火山杂岩体 角砾岩筒型金矿床 地质特征 成矿规律
修稿时间:2001-03-16

The geological characteristics of the mineralization of Zhuojiazhuang Gold Deposit, Pingyi County
Zhu Deping et al.. The geological characteristics of the mineralization of Zhuojiazhuang Gold Deposit, Pingyi County[J]. Gold, 2001, 22(8): 11-14
Authors:Zhu Deping et al.
Abstract:Zhuojiazhuang Gold Deposit is a small sized one which is related to secondary volcanic rock complex mass (monzodioritic porphyrite,monzonitic porphyry) of mesozoic era.Its pillar shaped orebody is strictly controlled by concealed breccia chimney.From center to outer of the breccia chimney,the grain size and composition of breccia and the composition and alteration of cementing materials all appear as zonal distribution.In this paper,the geological characteristics of gold deposit are described,the regularity of the mineralization of the gold deposit is summarized and the mineralizing vista in mining area is prognosticated.
Keywords:secondary volcanic rock complex mass  breccia chimney typed gold deposit  geological characteristic  re gularity of mineralization  Zhuojiazhuang
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号