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江西石城楂山里萤石矿床地质特征及成因探讨 预览

The geological characteristics and genesis discussion of Zhashanli fluorite deposit in Shicheng country, Jiangxi province
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摘要 楂山里萤石矿区处于武夷山成矿带,武夷山成矿带是我国十九个重要成矿带之一,分布着众多的萤石、叶腊石、石墨等非金属矿床及钨锡铜铅锌银等多金属矿床,矿床类型多样。本文在讨论楂山里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,对武夷山成矿带下一步寻找萤石矿床具有指导意义。 Zhashanli fluorite ore is located in Wuyishan metallogenic belt, that one of the nineteen important metallogenic belt in China. there are many fluorite, pyrophyllite, graphite and other non-metallic mineral deposits,also tungsten tin copper lead zinc silver and other metallic mineral deposits, various types of ore deposits in there. Based on the discussion of geological characteristics of Zhashanli fluorite ore, genesis of deposit were discussed in this paper. It has a guiding significance for the next step to find fluorite deposit in Wuyishan metallogenic belt.
作者 庄贤贵 彭琳琳 刘庆鸿 杨锐 Zhuang Xiangui1 ,Peng Linlin1,2 ,Liu Qinghong1, Yang Rui1( 1. Southern Jiangxi Geological Survey Party of JBEDGMR, Ganzhou, 341000, jiangxi, China; 2. The College of Earth Science and Engineering, Nanjing University, Nanjing 210000, Jiangsu, China)
出处 《化工矿产地质》 CAS 2017年第2期65-71,共7页 Geology of Chemical Minerals
关键词 矿床特征 萤石矿 楂山里矿区 江西石城 the characteristics of deposit, fluorite ore, Zhashanli deposit, Shicheng County of Jinagxi Province
作者简介 庄贤贵(1961~)男,长期从事地质勘查工作,高级工程师
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