摘要
铜厂山铅锌矿产于中酸性侵入岩与大东厂组碳酸盐岩接触带的矽卡岩中靠大理岩一侧和空树河组碎屑岩与大东厂组碳酸盐岩断层接触带中。矿区共发现5条铅锌矿体,其中规模较大具工业价值的有2条。
The Tongchangshan Pb - Zn deposit is formed in the skam of contact between the intermidiate - acid intrusive rock and the Dadongehang Formation carbonate rock, which is more adjacent to the marble side, and in the fault contact between Kongshuhe Formation clastic rock and Dadongchang Formation carbonate rock. There are 5 Pb -Zn ore bodies discovered in this orefield, including 2 ore bodies with large scale and commercial value.
出处
《云南地质》
2009年第2期152-156,共5页
Yunnan Geology
关键词
铅锌矿体
矽卡岩型
控矿因素
铜厂山
云南腾冲滇滩
Pb-Zn Ore Body
Skarn Type
Factor of Ore Control
Tongchangshan
Diantan,Tengchong,Yunnan
