%0 Journal Article
%T Fluid inclusions and exhumation history of ultra-high-pressure metamorphic rocks at lanshantou in the Sulu terrane, southeastern Shandong province<br>鲁东南岚山头超高压变质岩流体包裹体特征与板片折返史
%A FAN HongRui GUO JingHui HU FangFang CHU XueLei JIN ChengWei State Key Laboratory of Lithosphere Evolution
%A Key Laboratory of Mineral Resources
%A Institute of Geology
%A Geophysics
%A Chinese Academy of Sciences
%A Beijing
%A China
%A <br>范宏瑞
%A 郭敬辉
%A 胡芳芳
%A 储雪蕾
%A 金成伟
%J 岩石学报
%D 2005
%I 
%X 鲁东南岚山头含柯石英榴辉岩主要产于花岗质片麻岩内,是苏鲁超高压变质带主要榴辉岩体密集分布区之一。流体包裹体研究表明,榴辉岩矿物及细脉石英中捕获有四种类型包裹体:在超高压-高压榴辉岩相条件下捕获的 N_2±CO_2包裹体;在高压榴辉宕重结晶阶段被捕获的 CO_2-H_2O 包裹体和含子矿物高盐度 H_2O 溶液包裹体:在超高压岩石折返过程中的最晚(角闪岩相退变质甚至更晚)阶段捕获的低盐度 H_2O 溶液包裹体。利用榴辉岩矿物及脉体石英中捕获的流体包裹体相互期次关系,可以对本区超高压变质作用板片折返过程中的流体演化史进行重建。
%K Fluid inclusion
%K Ultra-high-pressure metamorphic rock
%K Exhumation
%K Lanshantou
%K Sulu terrain<br>流体包裹体
%K 超高压变质岩
%K 折返
%K 岚山头
%K 苏鲁
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=C66DCF7E9ED46574&yid=2DD7160C83D0ACED&vid=659D3B06EBF534A7&iid=E158A972A605785F&sid=D3CBA54FACB30BD9&eid=9D30FB531DC548C0&journal_id=1000-0569&journal_name=岩石学报&referenced_num=3&reference_num=61