%0 Journal Article
%T Ebullition of the Residual Magma and Sn-W Mineralization<br>残浆沸腾与锡钨成矿作用
%A JIN Ming-xi
%A WANG Jie-min
%A GAO Jin-xi
%A <br>金明霞
%A 王洁民
%A 高锦曦
%J 地球学报
%D 1999
%I 
%X A violent ebullition occurred in late residual magma of the S_type granite related to.Sn-W mineralization,and induced the generation of Sn and W ore_forming fluids of high temperature,high pressure,high salinity and high density.The fluids followed a path of stress difference,temperature difference,salinity difference and density difference for lateral migration or vertical migration in a relatively enclosed environment.The physicochemical condition experienced a jumping mutation, so that fluids precipitated and formed deposits when they were transported to the place where stress was released.
%K residual magma ebullition
%K fluids migration
%K stress releasing
%K Sn and W mineralization<br>残浆沸腾
%K 流体运移
%K 应力释放
%K 锡钨成矿
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=8A5BBB6F6CE57A261947A398BD93CD92&yid=B914830F5B1D1078&vid=A04140E723CB732E&iid=38B194292C032A66&sid=FDC7AF55F77D8CD4&eid=273ADA1BCEFE8C00&journal_id=1006-3021&journal_name=地球学报&referenced_num=1&reference_num=6