The Metallogenetic Geological Conditions of Maanshan Fe Deposit in <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:City w:st="on">Malong</st1:City>, <st1:State w:st="on">Yunnan Province</st1:State></st1:place>

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The Metallogenetic Geological Conditions of Maanshan Fe Deposit in Malong, Yunnan Province

详细信息

责任者：Chen Wei (Geological Team 317 ; Yunnan Bureau of Nonferrous Geology ; Qujing 655000 ; China)
刊名：Yunnan Geology
出版年：2011
卷期：30(3)
关键词：铁矿 ; iron ores ; 云南 ; Yunnan Province
页码：p.326-328
图表：1 illus., 2 refs.
分类号：1001
issnNo：ISSN1004-1885
isbnNo：CN53-1041/P

摘要

///The Fe deposit is formed by the pyrite and siderite in the basement rock because of the transportation and sedimentation after the surface weathering and leaching processes. It is a limonite deposit of weathering sedentary type.