首页 | 本学科首页   官方微博 | 高级检索  
     

湖南杨林坳钨矿床控矿构造地质地球化学特征浅析
引用本文:郑平, 黄满湘. 湖南杨林坳钨矿床控矿构造地质地球化学特征浅析[J]. 华北地质, 2011, (3): 198-202. doi: 10.3969/j.issn.1672-4135.2011.03.005
作者姓名:郑平  黄满湘
作者单位:湖南工程职业技术学院资源工程系,湖南长沙,410151; 中南大学地球科学与信息物理学院,湖南长沙,410083
基金项目:校企合作横向项目:湖南衡南杨林坳钨矿床成矿研究及找矿预测
摘    要:笔者在查明杨林坳白钨矿矿床地质特征的基础上,着重研究了控矿构造地球化学特征、矿化富集与构造的关系,矿体主要分布于F24断层上盘,矿化富集在杨林坳组砂岩和板溪群板岩的不整合面附近。矿体的空间分布与矿化富集规律明显受构造控制。

关 键 词:控矿构造   地球化学   不整合面   构造破碎带   杨林坳钨矿床

Geochemical Features of the Ore-control Structures in the Yanglin'ao Tungsten Deposit,Hunan Province
Geochemical Features of the Ore-control Structures in the Yanglin'ao Tungsten Deposit,Hunan Province[J]. North China Geology, 2011, (3): 198-202. doi: 10.3969/j.issn.1672-4135.2011.03.005
Authors:ZHENG Ping  HUANG Man-xiang
Affiliation:ZHENG Ping1,HUANG Man-xiang2(1.Resource Engineering Department of Hunan Engineering Profession College,Changsha Hunan 410151,China,2.Earth Science and Information Physics College,Central South University,Changsha Hunan 410083,China)
Abstract:Based on the geological features of the Yanglin' ao tungsten deposit,the authors mainly study the relationship between the geochemical features among the ore-control structures,mineralization enrichment and the structures.The orebodies distribute mainly in the up wall of the F24 faults,and the mineralization enrichment mostly occurs in the unconformity surface of the Yanglin' ao Group sandstone and Banxi Group slate hereabout.The orebody space distribution and the mineralization enrichment rules are controlled by the structures obviously.
Keywords:ore-control structure  geochemistry  unconformity surface  structural fracture belt  Yanglin'ao tungsten deposit
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《华北地质》浏览原始摘要信息
点击此处可从《华北地质》下载全文
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