摘要
本文在论述矿床的矿体形态、矿石矿物成分、化学成分、矿石结构、构造、矿物生成顺序及围岩蚀变等特征的基础上,提出矿床成因类型属“侧分泌矿床”。
Basing upon describing the orebody form; mineralogy, chemistry, texture and structure of ore; mineral paragenesis and wall-rock alteration, etc. of the deposit, this paper regards it as a deposit of lateral secretion genesis type.
出处
《云南地质》
1993年第4期352-356,351,共6页
Yunnan Geology
