摘要
云县邦六矿区铅锌矿体,均呈脉状产于不同的断层破碎带中,多期次的岩浆侵入活动,为矿体的形成提供了成矿物质的主要来源。矿床成因为中—低温构造岩浆热液矿床。
The ore body of Bangliu Pb-Zn orefield in Yunxian is veined in different fault fracture zone. The polyphasic magmatic intrusion provides the main material source for the formation of ore body. It is the middle-low T structure magmatic hydrothermal deposit in genesis.
出处
《云南地质》
2016年第1期59-63,共5页
Yunnan Geology
关键词
构造控矿
热液矿床
云南云县邦六
Ore Control of Structure
Hydrothermal Deposit
Bangliu, Yunxian, Yunnan
