摘要
莲花山萤石矿床是一个规模大，品位富，矿体相对集中，易采选，较富经济价值的矿床。矿床位于花岗岩体的内接触带，花岗岩体及ＮＥ向断裂同时控制着矿体的产出。矿石类型以单一萤石型为主，次为石英一萤石型。矿体与围岩界线清晰，属中－低温热液充填型矿床。
Lianhuashan fluorite deposit is characterized by a large scale, high grade, being easily mined and very valuable. It occurs in the endocontact of granitic body. And the occurrence of the ore body was synchronously controlled by the granitic body and NE-striking fault. The ore type is dominated by single fluorite-type, secondly, quartzfluorite type. The boundary line between ore body and country rock is distinct, being a meso-epithermal filling deposit.
出处
《江西地质》
1996年第2期85-92,共8页
Jiangxi Geology
