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长阳县竹林口铅锌矿成因探讨
引用本文:冉瑞生,刘圣德,杨文学.长阳县竹林口铅锌矿成因探讨[J].资源环境与工程,2009,23(3):219-224.
作者姓名:冉瑞生  刘圣德  杨文学
作者单位:湖北省宜昌地质勘探大队,湖北,宜昌,443100
摘    要:长阳县竹林口铅锌矿是2006~2008年湖北省地质勘查基金项目发现的,是继长阳背斜东段何家坪、王家湾铅锌矿之后发现的层控热液型铅锌矿床,在成矿地质背景、控矿构造条件等方面有相似之处,分析研究其成因机制,对长阳地区铅锌矿找矿工作具有指导意义.从地质结构、矿体地质特征、岩石地球物理特征等方面对竹林口铅锌矿进行分析,探讨其成矿机制和成矿环境,总结其成矿规律,为该区进一步开展地质工作提供参考.

关 键 词:竹林口铅锌矿  地质特征  成矿环境  成因类型

Discuss on Genesis of Zhulinkou Lead-Zinc Deposit in Changyang County
RAN Ruisheng,LIU Shengde,YANG Wenxue.Discuss on Genesis of Zhulinkou Lead-Zinc Deposit in Changyang County[J].Resources Environment & Engineering,2009,23(3):219-224.
Authors:RAN Ruisheng  LIU Shengde  YANG Wenxue
Affiliation:Yichang Brigade of Geological Exploration;Yichang;Hubei 443100
Abstract:The Zhulinkou lead-zinc deposit is discovered by Geological Survey Fund Project of Hubei Province from 2006 to 2008,As a typical stratabound hydrothermal deposit,it is found after deposits of Hejiaping and Wangjiawan in east segment of Changyang Anticline,several similarities between them in metallogenic geological background and ore-controlling structure conditions.The study on its genetic mechanism can guide the future prospecting in Changyang.Therefore,the Qiqiu lead-zinc deposit is analyzed from some as...
Keywords:Zhulinkou lead-zinc deposit  geological characteristics  metallogenic environment  genetic type  
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