摘要
盐源喜马拉雅期石英二长斑岩群和斑岩铜矿的发现和肯定，结束了康滇地轴中段攀西地区无喜马拉雅期斑岩和斑岩铜矿的历史。对认识该区大陆板内岩浆成矿作用及找矿工作具有特殊意义。本文就其地质特征及找矿前景作扼要介绍。
The discovery of beschtauite group and porphyry copper deposit in the Himalayan epoch in Yanyuan is of importance to understanding of continental intraplate magmatic ore-formation and ore-finding in Panzhihua-Xichang region in the middle sector of Kangdian axis. This paper discusses their geological features and ore content .
出处
《四川地质学报》
1995年第4期283-293,共11页
Acta Geologica Sichuan
关键词
喜马拉雅期斑岩群
青盘岩化带
斑岩型铜矿床
porphyry group in Himalayan epoch, propylitization, porphyry copper deposit.
