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额济纳旗灰石山东北铌多金属矿床成矿规律及成因浅析
引用本文:刘强,杨富林,袁晓鹏.额济纳旗灰石山东北铌多金属矿床成矿规律及成因浅析[J].地质找矿论丛,2018,33(1):41-45.
作者姓名:刘强  杨富林  袁晓鹏
作者单位:内蒙古地质矿产勘查院;
基金项目:市场项目"内蒙古自治区额济纳旗灰石山东北铌多金属矿勘探"资助。
摘    要:通过对灰石山东北铌多金属矿床地质特征综合分析表明,矿床的产出受地层和构造的双重制约。矿区的二叠系双堡塘组是矿源层,矿体具有明显的层位控制性;北东东向断裂构造提供了热液通道并进行了叠加改造;矿床成因类型属于沉积变质-热液叠加型。

关 键 词:灰石山铌多金属矿  二叠系双堡塘组  北东东向同生断裂  沉积变质-热液叠加型  内蒙古
收稿时间:2016/4/20 0:00:00
修稿时间:2017/6/28 0:00:00

Analysis of the metallogenic law and genesis of Niobium Polymetallic deposit in Northeast of Huishishan, Ejinaqi Banner
LIU Qiang,YANG Fulin and YUAN Xiaopeng.Analysis of the metallogenic law and genesis of Niobium Polymetallic deposit in Northeast of Huishishan, Ejinaqi Banner[J].Contributions to Geology and Mineral Resources Research,2018,33(1):41-45.
Authors:LIU Qiang  YANG Fulin and YUAN Xiaopeng
Institution:Inner Mongolia Institiute of Geology and Mineral Resourse Exploration, Hohhot 010010, China,Inner Mongolia Institiute of Geology and Mineral Resourse Exploration, Hohhot 010010, China and Inner Mongolia Institiute of Geology and Mineral Resourse Exploration, Hohhot 010010, China
Abstract:Comprehensive analysis of geological characteristics of Niobium polymetallic deposit in northeast of Huishishan mountain shows that the deposits is controlled by both the strata and structure. The Shuangbaotang Formation is the source bed. The ore bodies are stratabound. NEE fault is the hydrothermal fluid passageway where ore is formed in the source bed. Genetically the deposit is sedimentary metamorphic deposit reworked by hydrothermal fluid.
Keywords:Huishishan Niobium Polymetallic deposit  the Permian Shuangbaotang Formation  the NEE syngenetic faults  sedimentary and metamorphic deposit reworked by hydrothermal fluid
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