摘要
富源县老厂萤石矿矿体呈似层状,一是沿断层破碎带分布,二是沿二叠系龙潭组与阳新组两者之间的假整合接触界面展布,矿体主要受构造控制,该萤石矿属碳酸盐岩中的热液充填(交代)型矿床。
The ore body of laochang fluorite deposit in Fuyuan, Yunnan is stratoid either distributed along fracture zone or extended on the disconformity contact between Permian Longtan Formation and Yangxin Formation.The ore body is mainly controlled by the structure. It is a hydrothermal filling （ metasomatic ） fluorite deposit in the carbonate rock.
出处
《云南地质》
2017年第3期394-397,共4页
Yunnan Geology
关键词
构造控矿
热液充填型矿床
云南富源
老厂
Ore Control of Structure
Hydrothermal Filling Deposit
Laochang, Fuyuan, Yunnan
