摘要
在华北板块南缘熊耳群火山岩的矿化部位,普遍存在着特征明显的杏仁体,有的杏仁体甚至构成了矿化体,前人对此研究很少。对杏仁体的结构、构造特征及充填矿物进行了系统研究,详细论述了杏仁体的形成机制及其与成矿热水流体和成矿作用的关系,指出杏仁体是在华北板块南缘熊耳群火山岩内进行找矿勘查的重要标志。
Amygdales with distinct features are prevalent in mineralized sites in the Xiong'er Group vol-canic rocks on the southern margin of the North China plate.Some amygdales even have developed into mineralized bodies.However,previously this phenomenon was less studied.Based on a systematic study of the textures and structures of amygdales and their filling minerals,the formation mechanism of amygdales and their relationships with hydrothermal ore fluids and ore-forming processes are discussed in details in the paper.Finally,the authors point out that amygdales are an important indicator of exploration in the Xiong'er Group volcanic rocks on the southern margin of the North China plate.
出处
《地质通报》
CAS
CSCD
北大核心
2003年第5期356-363,共8页
Geological Bulletin of China
基金
国家自然科学基金项目(编号:40073013)
国土资源部自由探索项目(编号:2000440)资助。
关键词
华北板块南缘
熊耳群火山岩
杏仁体
热水流体
充填作用
交代作用
southern margin of the North China plate
Xiong'er Group volcanic rocks
amygdale
hy-drothermal fluid
cavity filling
metasomatism
