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北武夷葛山坞萤石矿床地质特征及成因探讨
引用本文:李康东,吴德来,华嵘辉,秦志刚,徐庆胜.北武夷葛山坞萤石矿床地质特征及成因探讨[J].资源调查与环境,2012(3):163-167.
作者姓名:李康东  吴德来  华嵘辉  秦志刚  徐庆胜
作者单位:江西省地质矿产勘查开发局赣东北大队
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。

关 键 词:北武夷  葛山坞  萤石矿  成因探讨

Geological characteristics and genesis of Geshanwu fluorite deposit in the northern Wuyishan
LI Kang-dong,WU De-lai,HUA Rong-hui,QIN Zhi-gang,XU Qing-sheng.Geological characteristics and genesis of Geshanwu fluorite deposit in the northern Wuyishan[J].Resources Survey & Environment,2012(3):163-167.
Authors:LI Kang-dong  WU De-lai  HUA Rong-hui  QIN Zhi-gang  XU Qing-sheng
Institution:(Northeast Jiangxi Geological Party;Jiangxi Bureau of Geology and Mineral Exploration and Development,Shangrao 33400,China)
Abstract:Wuyishan metallogenic belt is one of the most important metallogenic belts in China,where distributed amounts of fluorite,pyrophllite,graphite nonmetallic deposits and copper,lead,zinc and silver polymetallic 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.
Keywords:northern Wuyishan  Geshanwu  fluorite deposit  genesis
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