我国岩金成矿的基本规律  

The basic law of ore goldmineraliging in China

作　　者：于又华[1,2,3] 祁风茹[1,2,3] 程玉明[1,2,3] 

机构地区：[1]中国科学院资源环境科学信息中心 [2]中国科学院资源环境局 [3]吉林省有色地勘局

出　　处：《黄金科学技术》1999年第3期21-25,共5页Gold Science and Technology

基　　金：中国科学院"九五"重大攻关项目资助

摘　　要：有成矿远景的金矿集中区几乎都分布在大陆边缘构造活动带上，大型、特大型金矿床的形成改造与构造边缘活动带的发展、演化几乎同步。我国有成矿远景的金矿集中区，都与特定的含金岩系密切相关，具有明显的区域性与层控性。热活动中心。Gold fields with the minerogenetic prospects are mostly distributed in the active structure zones on the continental margins. The formations and doformations of the Largescale or extra largescale gold deposits are almost simultaneous with the development and evolution of the mobile zones on the structural margins. The gold depositconcentrations, which are possessed of the minerogenetic prospects, are closely interrelated with the specific auriferous rock series in China, having the distinctive charactrevistics of regin and formationcontrol. The existence of the centres of heat action and fields of heat fluid is a prerequisite for forming the concentrative regions of gold deposits with prospects.

关 键 词：岩金 成矿规律 含金岩系 金矿床 

分 类 号：P618.510.1[天文地球—矿床学] P612[天文地球—地质学]