北武夷葛山坞萤石矿床地质特征及成因探讨

详细信息

刊出日期: 2012-09-15

Geological characteristics and genesis of Geshanwu fluorite deposit in the northern Wuyishan

Publish Date: 15 September 2012

摘要: 武夷山成矿带是我国十九个成矿带之一,分布着众多的萤石、叶腊石、石墨等非金属矿床及铜铅锌银等多金属矿床,矿床类型多样。本文在讨论葛山坞萤石矿成矿地质特征的基础上,对该矿床的成因进行了探讨,对北武夷地区下一步寻找萤石矿床具有指导意义。
- 北武夷 /
- 葛山坞 /
- 萤石矿 /
- 成因探讨
Abstract: Wuyishan metallogenic belt is one of the most important metallogenic belts in China, where distribut- ed amounts of fluorite, pyrophllite, graphite nonmetallic deposits and copper, lead, zinc and silver poly- metallic deposits with various genetic types. Based on analysing metallogenetic geological characteristics of the Geshanwu fluorite deposit, this paper systematically discusses the genesis of the deposit, which will provide direction for prospecting fluorite deposit in the northern Wuyishan.