摘要
金矿受构造破碎带控制,与岩浆热液活动及地下热卤水溶滤作用有关的热液型金矿床。分出三种蚀变型矿石,自然金为主,少量磁铁矿、黄铁矿含金。
The Au is a Au deposit of hydrothermal type related to the hydrothermal activity of magma and leaching effect of underground thermal brine, which is controlled by the structural fracture zone, and can be divided into 3 alteration ore types, ie, major native Au, minor Au -bearing magnetite, pyrite.
出处
《云南地质》
2013年第2期133-135,共3页
Yunnan Geology
关键词
三类蚀变岩含金
破碎带控矿
岩浆热液供矿
康廓组赋矿
云南剑川段家登
3 Types of Au-Bearing Alteration Rock
Ore Control of Fracture Zone
Ore Supply of Magmatic Thermal Fluid
Ore-Bearing Kangkuo Formation
Duangjiadeng
Jianchuan
Yunnan
