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湖北青峰断裂带构造特征及其铅锌矿床的成因分析
引用本文:赵前禹,伍静华,吴贤亮,宁红辉,谢芳斌. 湖北青峰断裂带构造特征及其铅锌矿床的成因分析[J]. 资源环境与工程, 2006, 20(1): 13-18
作者姓名:赵前禹  伍静华  吴贤亮  宁红辉  谢芳斌
作者单位:鄂西北地质矿产调查所,湖北,襄樊,441003;鄂西北地质矿产调查所,湖北,襄樊,441003;鄂西北地质矿产调查所,湖北,襄樊,441003;鄂西北地质矿产调查所,湖北,襄樊,441003;鄂西北地质矿产调查所,湖北,襄樊,441003
基金项目:在撰写本文过程中得到蔡志勇高级工程师的精心指导、刘兴义高级工程师和湖北省地调院鄂西地调分院的支持和帮助.王宗合教授级高级工程师审阅了全文,刘源骏教授级高级工程师提出了宝贵的修改意见.在此表示衷心的感谢!
摘    要:阐述青峰断裂带构造特征及变形机制,分析与断裂带有关的铅锌矿床地质特征,对其控矿因素、成矿模式作了初步探讨,并首次阐明该区铅锌矿床为沉积喷流~改造型矿床。总结出了改造富集成矿期的矿床地质特征和找矿标志,提出了新的找矿靶区,为本区寻找铅锌多金属矿床提供了新的思路和找矿方向。

关 键 词:断裂带  变形机制  铅锌  控矿因素  成矿模式
文章编号:1671-1211(2006)01-0013-06
收稿时间:2005-06-20
修稿时间:2005-08-23

THE QINGFENG FAULT AND ITS RELATIONS WITH LEAD-ZINC DEPOSITS IN HUBEI
Zhao Qianyu,Wu Jinghua,Wu Xianliang,Ning Honghui,Xie Fangbing. THE QINGFENG FAULT AND ITS RELATIONS WITH LEAD-ZINC DEPOSITS IN HUBEI[J]. Resources Environment & Engineering, 2006, 20(1): 13-18
Authors:Zhao Qianyu  Wu Jinghua  Wu Xianliang  Ning Honghui  Xie Fangbing
Abstract:This paper deals with the structural characteristics and deformation of the Qingfeng fault and its related lead-zinc deposits.The ore-controlling factors and metallurgical model have been discussed.It is considered that the deposits are from sedimentary eruption reformed ones.The features of the deposits and the indicators for prospecting have also been summed up.The target areas for further investigation have been put forward.
Keywords:fault zone  deformation mechanism  lead-zinc  ore-controlling factors  metallurgical model
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