摘要
保山市小松林铅锌多金属矿,矿体呈脉状、似层状赋存于近南北向断裂破碎带中矿体近矿围岩为为上寒武统核桃坪组第三段之大理岩化灰岩。该矿床为中低温热液充填(交代)型含金铅锌矿床。
The ore body of Xiaosonglin Pb-Zn multimetallic deposit is veined, stratoid, in near NS fault zone. The wall rock near ore body Upper Cambrian Hetaoping Formation 3^（rd）Member marblization limestone. It is a middle-low T hydrothermal filling（ metasomatism） type Au-bearing Pb-Zn deposit.
出处
《云南地质》
2017年第2期241-244,共4页
Yunnan Geology
关键词
构造控矿
中低温热液矿床
云南保山小松林
Ore Control of Structure
Middle-Low T Hydrothermal Deposit
Xiaosonglin
Baoshan
Yunnan
