摘要
东准噶尔强应变构造带是板块碰撞作用的产物 ,控制了金成矿带的分布 ,而金的矿化富集地段分布于强应变构造带与走向北北西的断裂交汇部位。金矿体及矿脉则形成于强应变构造带的次级断裂和裂隙中。
Eastern Junggar highly strained structural belt is a product of plate collision. Distribution of eastern Junggar gold deposit is controlled by this highly strained structural belt. Gold mineralization is much more developed in intersection parts of the highly strained structural belt and NNW trending faults. Gold ore bodies and veins are developed in subsidiary fractures and fissures which are located in the highly strained structural belt.
出处
《地质与勘探》
CAS
CSCD
北大核心
2000年第3期15-17,21,共4页
Geology and Exploration
基金
国家"九.五"科技攻关项目!( 96-915 -0 2 -0 6-0 1)
关键词
东准噶尔
板块碰撞
强应变构造带
金矿床
eastern Junggar, plate collision, highly strained structural belt, gold deposit
