摘要
乐红铅锌矿位于扬子准地台西缘、滇东台褶带滇东北台褶束内。矿区内一组北西向高角度断层暨组成矿区的主体构造格架,又是矿体的主要控矿构造,同时铅锌矿化与震旦系灯影组上段(Z2dn2)白云岩关系十分密切。
Lehong Pb-Zn deposit is in the NE Yunnan platform fold bundle of E Yunnan platform fold belt of the W margin of Yangzi paraplatform. The main structure framework of orefield is a set of NW high angle faults, which is also the structure of ore control. And the Pb-Zn metallogenesis is in close relation with Sinian Dengying Formation upper member （Z2dn2） dolomitite.
出处
《云南地质》
2016年第3期349-353,共5页
Yunnan Geology
关键词
构造控矿
矿源层
云南乐红
Ore Control of Structure
Ore Source Bed
Lehong, Yunnan.
