摘要
通过对华南地区紫金山、银山、铜厂等典型矿床在成矿条件、矿床地质特征、成矿物理化学环境等方面的综合对比，指出它们同属“火山─斑岩”成矿系列，且系垂向上不同就位深度层次上的产物，进而提出“火山─斑岩”成矿系列的成矿模式。
Through the comparison of their metallogenic conditions, ore-forming physicochemical environments and geologic characteristics, Zijingshan, Yinshan and Tongchang ore deposits were considered as a metallogenic series of 'Volcanic-Porphyry' and as the productions of magma occurrence at different depth. Futhermore,the metallogenic model of 'Volcanic-Porphyry' metallogenic series was proposed.
出处
《中国有色金属学报》
EI
CAS
CSCD
1996年第1期11-16,共6页
The Chinese Journal of Nonferrous Metals
关键词
火山斑岩型
成矿
模式
矿床
地质特征
金属矿
volcanic-porphyry metallogenic series
occurrence depth
metallogenic model
