摘要
金矿体赋存于二叠系中统吴家坪组与辉长、辉绿岩体的接触带中,或产于辉长、辉绿岩体内的断层破碎带内,为一构造控制的热液蚀变型金矿床。
The Au orebody is in the contact zone between Middle P Wujiaping Formation and gabbro- diabase or in the fault zone of gabbro- diabase body. It is a hydrothermal alteration Au deposit controlled by the structure.
出处
《云南地质》
2015年第4期539-542,共4页
Yunnan Geology
关键词
岩体接触带
断层破碎带
热液蚀变型金矿
云南富宁县弄歪
Contact of Rock Body
Fault Fractured Zone
Hydrothermal Alteration Au Deposit
Longwai
Funing
Yunnan