首页 | 本学科首页   官方微博 | 高级检索  
     检索      

漓渚铁矿东矿成矿地质特征及控矿因素分析
引用本文:范效仁,夏国强,谢纪荣,马正平.漓渚铁矿东矿成矿地质特征及控矿因素分析[J].矿产与地质,2009,23(6):538-541.
作者姓名:范效仁  夏国强  谢纪荣  马正平
作者单位:浙江有色地质矿产勘查院,浙江,绍兴,312000
基金项目:全国危机矿山接替资源找矿项目 
摘    要:漓渚铁矿是一个以铁为主,共(伴)生锌钼的矽卡岩型贫磁铁矿矿床,铁矿体均分布于震旦系西峰寺组白云质灰岩和寒武系灰岩内沿断裂构造发育的含矿矽卡岩带中,呈似层状、透镜状,其形态、规模、矿化特征及成矿元素组合受NE向断裂控制,与广山花岗岩体关系密切。

关 键 词:铁矿床  地质特征  矽卡岩型  控矿因素  漓渚  浙江

Geological characteristics and ore-controlling factors analysis in eastern Lizhu iron deposit
FAN Xiao-ren,XIA Guo-qiang,XIE Ji-rong,MA Zheng-ping.Geological characteristics and ore-controlling factors analysis in eastern Lizhu iron deposit[J].Mineral Resources and Geology,2009,23(6):538-541.
Authors:FAN Xiao-ren  XIA Guo-qiang  XIE Ji-rong  MA Zheng-ping
Institution:(Zhejiang Survey Institute of Nonferrous Metal Mineral Resources and Geology, Shaoxing, Zhejiang 312000)
Abstract:Lizhu iron orefield is an iron-based skarn-type poor magnetite deposits with zinc and molybdenum associated minerals. Iron ore bodies are distributed in ore-bearing skarn belt along the fault structure in dolomitic limestone of Xifengsi group of Sinian system and limestone of Cambrian system, which is stratiform-like and lenticular orebody. Its shape, scale, mineralization and ore-forming elements are controlled by the NE-trending fault and it has closely relationship with Guangshan granite.
Keywords:eastern Lizhu iron deposit  skarn-type  iron orebody  ore-controlling factors
本文献已被 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