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新疆哈密天湖铁矿床地质特征及成因分析
引用本文:米登江,邹存海,张江,唐小东. 新疆哈密天湖铁矿床地质特征及成因分析[J]. 地质找矿论丛, 2014, 29(2): 223-229
作者姓名:米登江  邹存海  张江  唐小东
作者单位:中国冶金地质总局新疆地质勘查院,乌鲁木齐830063
摘    要:哈密天湖铁矿是新疆东天山地区的一个大型铁矿床。天湖铁矿床产出在新元古界天湖群第三组变质岩系中,铁矿体赋存于白云质大理岩内并呈层状、似层状产出;碳酸盐岩蚀变部位的部分铁矿石变富,且有黄铜矿、闪锌矿等硫化物生成。矿石组构方面,具有细-中细粒状结构、网格状结构、残余结构,层状、条带状构造。矿床成因类型属于沉积变质-区域混合岩化热液叠加改造型。

关 键 词:天湖铁矿  矿床地质特征  矿床成因  沉积变质  热液叠加改造  新疆
收稿时间:2013-11-14

Geological characteristics and genetic analysis of Tianhu iron deposit in Hami area, Xinjiang
MI Dengjiang,ZHOU Chunhai,ZHANG Jiang and TANG Xiaodong. Geological characteristics and genetic analysis of Tianhu iron deposit in Hami area, Xinjiang[J]. Contributions to Geology and Mineral Resources Research, 2014, 29(2): 223-229
Authors:MI Dengjiang  ZHOU Chunhai  ZHANG Jiang  TANG Xiaodong
Affiliation:MI Dengjiang(Xinjiang Geological Exploration Institute, China Bureau of Metallurgical Geology and Exploration, Wulumuqi 830063, Xinjiang, China) ZHOU Chunhai(Xinjiang Geological Exploration Institute, China Bureau of Metallurgical Geology and Exploration, Wulumuqi 830063, Xinjiang, China) ZHANG Jiang(Xinjiang Geological Exploration Institute, China Bureau of Metallurgical Geology and Exploration, Wulumuqi 830063, Xinjiang, China) TANG Xiaodong(Xinjiang Geological Exploration Institute, China Bureau of Metallurgical Geology and Exploration, Wulumuqi 830063, Xinjiang, China)
Abstract:Tianhu iron deposit is a large-sized iron deposit occurring in the third metamorphic rock series of Proterozoic Tianhu group.Ore bodies are layered or layeroid in dolomitic marble.At position where the marble is overprinted and altered by hydrothermal fluid the iron ore gets richer chalcopyrite and sphalerite are formed.The ore is in fine-medium fine,grid and residual texture and layering and banding structure.It is genetically a sedimentary-metamorphosed-hydrothermally reworked iron deposit.
Keywords:Tianhu iron deposit  characteristics of the deposit  genesis of the deposit  sedimentary-metamorphism  hydrothermal reworking  Xinjiang
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