板块构造环境对金矿成矿的控制作用  

SPECIALIZATION AND CONTROL OF PLATE TECTONIC ENVIRONMENT ON GOLD METALLIZATION

作　　者：葛良胜[1] 武玉海[1] 

机构地区：[1]黄金地质研究所

出　　处：《黄金地质》1996年第3期6-13,共8页Gold Geology

摘　　要：以板块构造理论为基础，论述了板块构造与金矿成矿的关系，指出与金矿有关的主要板块构造环境是裂谷带、岛弧地带、深大断裂带和碰撞带，不同大地构造环境对金矿成矿的控制具有不同的特点。另一方面，不同板块构造环境对金矿成矿具有专属性，这种专属性随着板块间的相互作用及其旋回性发展具有时空复合特征。The relations between plate tectonics and gold metallization are discussed on the basis of the plate tectonic theory. The major plate tectonic environments related to gold deposit are rift zone,island arc belt,collision zone and deep-fracture zone,the controls of different geotectonic environments on gold metallization have different characters.On the other hand,every environment has a specialization for gold metallization,with the interaction between plates and its cyclicity development,this specialization has a time-spece complex signature.

关 键 词：板块构造 成矿专属性 金矿床 构造环境 

分 类 号：P618.510.5[天文地球—矿床学]