%0 Journal Article
%T Characteristics and genesis of ore tube structure of Tamu zinc-lead deposit, southwest margin of Tarim Basin, Xinjiang<br>新疆塔里木盆地西南缘塔木铅锌矿床矿石管状构造特征与成因
%A YANG XiangRong
%A PENG JianTang
%A HU RuiZhong
%A QI HuaWen
%A LIU Shen
%A <br>杨向荣
%A 彭建堂
%A 胡瑞忠
%A 戚华文
%A 刘燊
%J 岩石学报
%D 2009
%I 
%X Based on the observation of hand specimens and microscopic scale section samples, the tube structure ores show axissymmetric characteristics in Tamu zinc-lead deposit. This structure is resulted from dissolution and metasomatism, which reflect the sulfide mineralization (sphalerite) and dissolution (dolostone I) are contemporaneous and indicate mineralization relates to two processes dissolution-metasomatism and cavity filling. Moreover, the pulse-styled fluid movement induces the more complex axissymmetric tubes.
%K Tube structure
%K Genesis
%K Tamu zinc-lead deposit
%K Tarim Basin<br>管状构造
%K 成因
%K 塔木铅锌矿
%K 塔里木盆地
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=487B6368CD96957C0B16BF33F32825F1&yid=DE12191FBD62783C&vid=C5154311167311FE&iid=E158A972A605785F&sid=1BE4748776BF02C4&eid=88B4027FEBE4F5FF&journal_id=1000-0569&journal_name=岩石学报&referenced_num=3&reference_num=39