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中国火山岩地区金的成矿环境及分布规律
引用本文:王碧香,杨岳清,史仁灯,银剑钊,石森.中国火山岩地区金的成矿环境及分布规律[J].矿床地质,1997,16(1):11-20,40.
作者姓名:王碧香  杨岳清  史仁灯  银剑钊  石森
作者单位:[1]中国地质科学院地质研究所 [2]矿床地质研究所
基金项目:国家“八五”重点黄金科技攻关项目
摘    要:中国是一个火山岩广泛分布的国家,火山岩区的金矿不论其数量和储量在全国均占有重要地位,根据金和火山活动的关系,可划分出6种金矿类型,它们主要分布在6个火山岩区中,不同地区金的成矿作用各有其特色,总体可概括出7条成矿特征,这对于在我国广阔的火山岩区寻找金矿具有重要的指导意义。

关 键 词:火山岩  金矿床  成矿环境  分布规律

Geological setting and temporal-spatial distribution of gold deposits in volcanic terrains of China
Wang Bixiang ,Yang Yueqing ,Shi Rendeng ,Yin Jianzhao and Shi Sen.Geological setting and temporal-spatial distribution of gold deposits in volcanic terrains of China[J].Mineral Deposits,1997,16(1):11-20,40.
Authors:Wang Bixiang  Yang Yueqing  Shi Rendeng  Yin Jianzhao and Shi Sen
Institution:Wang Bixiang 1,Yang Yueqing 2,Shi Rendeng 1,Yin Jianzhao 2 and Shi Sen 3
Abstract:Volcanic rocks of various ages and their intrusive equivalents are widespread in China,with the existence of a great variety of rock associations. The distribution of various types of gold deposits is generally associated with the features of volcanic rock associations,i.e.,a particular type of gold deposit is related to a specific rock association. Large and supergiant gold deposits have been found in volcanic terrains. Through an intensive study of six genetic types of gold geposits in volcanic terrains,the authors have come to the conclusion that the principal metallogenic epoch of gold deposits in volcanic terrains of China is Mesozoic. Meso zoic gold deposits account for 61.3% of the total gold deposits in volcanic terrains and contribute 73% of the reserves. Late Paleozoic gold deposits are next in number and reserves. In terms of geographic distribution,Mesozoic gold deposits are dominant in eastern China(in volcanic terrains with metamorphosed basement),while Paleozoic ones predominate in western China.The most important gold deposits in China's volcanic terrains are of epithermal type. In comparison with the other five types,this type accounts for 47% of the total number and 44.3% of the total reserves. On the basis of the relations of the distribution of gold deposits to rock associations and structures in volcanic terrains,the authors advance the viewpoint of multifactor mineralization,i.e.,gold deposits are formed by circulation of hydrothermal fluids together with auriferous substances at the intersection of two sets of faults(or terranes).
Keywords:volcanic terrain  gold deposit  temporal spatial distribution  
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