胡文华,杨四春,冉华南.安徽绩溪荆州银多金属矿地质特征和控矿因素浅析[J].地质找矿论丛,2009,24(1):62-65,90
安徽绩溪荆州银多金属矿地质特征和控矿因素浅析
PRIMARY ANALYSIS OF GEOLOGICAL CHARACTERISTICS AND ORE-CONTROL FACTORS OF JINGZHOU Ag-POLYMETAL DEPOSIT IN JIXI AREA,ANHUI PROVINCE
投稿时间:2008-11-19  修订日期:2009-01-05
DOI:10.6053/j.issn.1001-1412.2009.1. 011
中文关键词:  荆州银多金属矿  地质特征  控矿因素  安徽省
英文关键词:Jingzhou Ag-polymetal deposit  geological feature  ore-control factor  Anhui province
基金项目:安徽省省级地质勘查项目专项费(2006-11)资助
作者单位
胡文华  
杨四春  
冉华南  
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中文摘要:
      安徽绩溪荆州银多金属矿产于蓝田组灰岩的似层状夕卡岩中,属于远离接触带的夕卡岩型矿床。蓝田组岩石中富含银、铜、铅、锌等元素,为银多金属矿的形成提供了矿质来源;区域上燕山期岩浆活动为矿床的形成提供了大量热源、成矿介质和部分矿源;适宜的褶皱构造和断裂构造则提供了矿液运移通道和矿质沉淀的空间。
英文摘要:
      Jingzhou Ag-polymetal deposit is located in the layered skarn of limestone of Lantian formation.Lantian formation is rich in Ag,Cu,Pb,Zn etc.and supplies ore materials for formation of the deposit and the regional Yanshanian magmatism the heat energy and the ore-forming media and some ore materials.The proper fold and fault provide passage and room for ore fluid transportation and accumulation.
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