摘要
鄂拉山口银铅锌矿床的发现,是近几年来在青海省鄂拉山成矿带上找矿的重大突破。矿床赋存于火山机构相的环形断裂构造和区域北西向断裂构造的交汇部位,矿体局限在次火山岩的侵入空间内,并定格在火山地震或次火山隐爆下的角砾岩带中。
Ag- Pb- Zn deposit discovered in Ela mountain pass , is a significant breakthrough in Ela Qinghai province Ela mountain mineralization belt e in recent few years. The deposit is located on the intersection of volcanic framework annular fault structure and region north and west fault structure , the ore body is limited in the volcanic intrusive space, and fixed in volcanic earthquake or volcanic breccia zone of hidden explosives.
出处
《黄金科学技术》
2007年第1期41-44,共4页
Gold Science and Technology
关键词
鄂拉山成矿带
火山构造
鄂拉山口银铅锌矿床
青海
Ela mountain
mineralization belt
Volcano structure
Ag- Pb -Zn deposit
in Ela mountain pass
Qinghai
