摘要
沧源芒哈铅锌银多金属矿床是澜沧江南段火山岩成矿带乃至三江地区较重要的一种新类型,矿体产于花岗斑岩脉的外接触带,岩体和矿体同受北西走向的构造破碎带控制。
The Mangha Pb - Zn - Ag muhimetallic deposit of Cangyuan is a rather importang new type in the volcanic metallogenetic zone of south section of Lancangjiang river, even in the San- jiang three- river area, which exists in the outer contact of granite porphyry vein. The rock body and ore body both are controlled by the NW structure fracture zone.
出处
《云南地质》
2008年第2期218-222,共5页
Yunnan Geology
关键词
铅锌银矿新类型
花岗斑岩脉
外接触带
沧源芒哈
New Type of Pb - Zn - Ag Deposit
Granite Porphyry Vein
Outer Contact
Mangha, Cangyuan
