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湖南姑婆山锡矿田地质特征及找矿前景
引用本文:邹建林,曾永红,陈文辉.湖南姑婆山锡矿田地质特征及找矿前景[J].华南地质与矿产,2005(2):45-52,67.
作者姓名:邹建林  曾永红  陈文辉
作者单位:湖南省地质调查院湘中矿产地质调查所,湖南,娄底,417000
基金项目:中国地质调查局国土资源大调查项目(200110200024).
摘    要:姑婆山锡矿田原生锡矿床的成因类型有构造蚀变带型、构造蚀变岩一矽卡岩复合型和接触带矽卡岩型3种。通过对各类锡矿成矿地质条件、控矿因素和成矿规律的分析与总结,认为岩浆岩是控制各类型锡矿形成和分布的首要条件,区域性NE至SN向断裂(F1、F2)为导矿、控矿构造,其旁侧的次级断裂及岩体与地层的接触带为容矿构造;提出矿田西部和北部具有良好的找矿前景。

关 键 词:锡矿田  找矿远景区  湖南姑婆山
文章编号:1007-3701(2005)02-0045-08
修稿时间:2005年4月20日

Geological characteristics and prospecting potential of the Guposhan tin orefield,southern Hunan Province
ZOU Jian-lin,ZEN Yong-hong,CHEN Wen-hui.Geological characteristics and prospecting potential of the Guposhan tin orefield,southern Hunan Province[J].Geology and Mineral Resources of South China,2005(2):45-52,67.
Authors:ZOU Jian-lin  ZEN Yong-hong  CHEN Wen-hui
Abstract:Primary tin deposits of Guposhan orefield in Hunan Province include structural alteration zone type,structural alteration zone-skarn composite type and contact skarn type. In the light of analyses and summarization of metallogenic conditions,ore-controlling factorsand mineralization regularities,the authors believe that granitic magmatism is the key factor for tin mineralization,the NE- to SN-striking faults(F_(1)and F_(2)) and their secondary faults are ore-control and host structures,respectively. Study shows that the western and northern part of the orefield have excellent prospecting potential.
Keywords:tin deposit  prospecting area  Guposhan  Hunan  
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