%0 Journal Article
%T Constraints of high-saline metamorphic fluids to gold deposits of greenstone belts in China.<br>高盐变质流体对我国绿岩带金矿的制约
%A Xie Yihan
%A Fan Hongrui Institute of Geology
%A Geophysics
%A Chinese Academy of Sciences
%A Beijing
%A Chin
%A The Research Center of Mineral Resources Exploration
%A Chinese Academy of Sciences
%A Beijing
%A China
%A <br>谢奕汉
%A 范宏瑞
%J 岩石学报
%D 2000
%I 
%X 高盐变质流体为绿岩带原岩在变质 -混合岩化过程中产生的液体 ,其含盐度高达 30～ 40 wt% Na Cl,富含 K、Na、Ca、Mg碱金属离子 ,K/ Na≈ 1,呈强碱性 ,有利于绿岩中 Au的活化和迁移 ,使绿岩带起到金的矿源层作用 ,并且间接地控制了变质期后绿岩型金矿的形成和分布 ,控制了绿岩型金矿的规模大小
%K High saline metamorphic fluid
%K Fluid inclusion
%K Greenstone belt
%K Gold deposit<br>高盐变质流体
%K 流体包裹体
%K 绿岩带
%K 金矿
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=4277269EFB882ACAA0E322CD4580AC22&yid=9806D0D4EAA9BED3&vid=7801E6FC5AE9020C&iid=E158A972A605785F&sid=8DDBA6455F2E3ECF&eid=66D0A4667FE1A38D&journal_id=1000-0569&journal_name=岩石学报&referenced_num=1&reference_num=4