摘要
桃花铁多金属矿与该区的次级构造、花岗斑岩、中等蚀变带等关系密切,经探矿工程控制其资源量已达小型规模,与花岗斑有关的断裂充填型矿床。
Taohua Fe multimetallic deposit is in close relation with the secondary structure,granite porphyry and middle class alteration zone,with a small scale of resource reserves according to the exploration engineering control.It is filling type with fulit in granite porphyry.
出处
《云南地质》
2013年第1期30-32,29,共4页
Yunnan Geology
关键词
中等蚀变带
次级构造
花岗斑岩
探矿工程控制
桃花铁多金属矿
Middle Class Alteration Zone
Secondary Structure
Granite Porphyry
Exploration Engineering Control
Taohua Fe Multimetallic Deposit
