陕西镇坪双河口铌矿床地质地球化学特征与成因探讨
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  • 英文篇名:Geological and Geochemical Characteristics and Genesis of the Shuanghekou Niobium Deposit in South Qinling,Shaanxi
  • 作者:朱伟 ; 郑婧 ; 刘新会 ; 陈应涛 ; 刘能 ; 康琴琴 ; 杨玲
  • 英文作者:ZHU Wei;ZHENG Jing;LIU Xin-hui;CHEN Ying-tao;LIU Neng;KANG Qin-qin;YANG Ling;Geological Survey Center in Shaanxi Province;No.5 Gold Geological Party of CAPF;Department of Geology and Environmental Engineering,Xi'an University of Science and Technology;
  • 关键词:铌矿床 ; 地球化学特征 ; 矿床成因 ; 粗面岩 ; 双河口 ; 镇坪县 ; 陕西
  • 英文关键词:niobium deposit;;geological and geochemical characteristics;;genesis;;trachyte;;Shuanghekou;;Zhenping county;;Shaanxi
  • 中文刊名:DZKT
  • 英文刊名:Geology and Exploration
  • 机构:陕西省地质调查中心;武警黄金第五支队;西安科技大学地质与环境学院;
  • 出版日期:2018-09-15
  • 出版单位:地质与勘探
  • 年:2018
  • 期:v.54;No.479
  • 基金:陕西省公益性地质工作项目(编号:20130101)资助
  • 语种:中文;
  • 页:DZKT201805005
  • 页数:11
  • CN:05
  • ISSN:11-2043/P
  • 分类号:55-65
摘要
为深入认识陕西双河口铌矿床的赋矿特征与矿床成因,本文进行详细的岩石学、矿物学、矿床地球化学研究。结合该区域已有的研究成果,认为镇坪双河口铌矿床是以铌为主的大型矿床,该矿床赋矿地层为奥陶系-志留系斑鸠关组,控矿构造为北西向次级断裂带,赋矿岩石以黑云母粗面岩为主,热液蚀变发育,铌矿化与钠长石化、钠铁闪石化、黑云母化关系密切。矿区粗面质火山岩富碱质,具有Eu负异常,含矿粗面岩富钠、轻稀土元素。矿床成因类型为岩浆热液型,早期岩浆结晶分异初步富集铌-稀土元素,岩浆期后碱质交代作用进一步富集成矿。
        In order to further understanding the mineralization characteristics and genesis of the Shuanghekou Nb deposit in Zhenping county,Shaanxi,we have made a detailed study on the petrology,mineralogy,and geochemistry of this area. In combination with the existing research results in this region,we suggest that this is a large-scale deposit dominated by niobium. The ore-bearing strata are Banjiuguan Formation of Ordovisn-Silurisn Systems. The ore controlling structure is a northwest trending secondary fault zone. The ore is dominated by biotite trachyte type niobium iron. The ore-hosting rock is biotite trachyte. The deposit developed a series of hydrothermal alteration. The Nb mineralization is closely related to the albitization and biotitization. The trachyte belongs to shoshonitic series with an Eu negative anomaly and is rich in light rare earth elements and Na_2O. The deposit is magmatic hydrothermal-type in genesis. The magma in the early stage of crystallization and differentiation processes had a preliminary enrichment of niobium-rare earth elements,while the later stage was further enriched and concentrated in ore-formation by alkali metasomatic alteration.
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