%0 Journal Article
%T Study on fluid inclusions and discussion on mechanism of hydrothermal mineralization of Manaoke gold deposit, north-western Sichuan province.<br>川西北马脑壳金矿床流体包裹体研究与热液成矿机理探计
%A Wang Keyong
%A Yao Shuzhen
%A Zhang Jun
%A Lu Xinbiao Changchun University of Science
%A Technology
%A Changchun
%A Chin
%A China University of Geosciences
%A Wuhan
%A China
%A <br>王可勇
%A 姚书振
%J 岩石学报
%D 2000
%I 
%X 系统的流体包裹体研究表明，马脑壳金矿床物石英中发育有液相，纯液相，含ＣＯ３三相，纯ＣＯ２相及含有机质等五种主要类开型的原生流体包裹体，其均一温度为１２０～３００℃，热液盐度为０．５～１１．０ｗｔ％ＮａＣｌ，密度为０．７８～０．９５ｇ／ｃｍ＾３，成矿压力为３２．８７～１１３．６１５ＭＰａ，主矿化阶段成矿认发生过明星的流体混合及相分离作用，由此导致含矿热液体纱Ｔ、ｐＨ、ｆｏ２及ｆｓ２等物化条件参数的降
%K Fluid inclusion
%K Hydrothermal mineralization mechanism
%K Fluid mixing and phase separation processes
%K Micro
%K grain disseminated gold deposit
%K North
%K western Sichuan province<br>流体包裹体
%K 热液成矿机理
%K 流体混合
%K 金矿床
%K 沉淀
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=64B658EDCDC71810&yid=9806D0D4EAA9BED3&vid=7801E6FC5AE9020C&iid=E158A972A605785F&sid=2497388423811B81&eid=6D6B4A516C7DB6EE&journal_id=1000-0569&journal_name=岩石学报&referenced_num=2&reference_num=4