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吉林省桦甸地区太古宙花岗质片麻岩的侵位与变形研究
引用本文:周永胜,林强.吉林省桦甸地区太古宙花岗质片麻岩的侵位与变形研究[J].吉林地质,1997,16(1):33-41.
作者姓名:周永胜  林强
作者单位:[1]国家地震局地质研究所 [2]长春科技大学
摘    要:根据岩石组合,分布,接触,包裹关系以及结构和构造,吉林省桦甸地区太古宙花岗质林岩为角闪英云闪长质片麻岩类和黑云母花岗闪长质片麻岩类,角闪英云闪长质片麻岩类为变形前侵入体,黑云母花岗闪长质片麻岩类为同变形侵入体,两类花岗质片麻岩的侵位是晚太古宙近东西向构造变形相伴生的岩浆活动事件。

关 键 词:太古宙  花岗质片麻岩  侵入体  变形  片麻岩

A STUDY ON THE EMPLACEMENT AND DEFORMATIONOF THE ACHEAN GRANITE GNEISS IN THEHUADIAN AREA,JILIN PROVINCE
Zhou,Yongsheng.A STUDY ON THE EMPLACEMENT AND DEFORMATIONOF THE ACHEAN GRANITE GNEISS IN THEHUADIAN AREA,JILIN PROVINCE[J].Jilin Geology,1997,16(1):33-41.
Authors:Zhou  Yongsheng
Abstract:According to rock association,distribution,contact relationship of enclosing,texture and structure in the Huadian,Jilin province,the Achean granite gneiss is classified into pladorite gneiss and boitite granite gneiss. The pladorite gneiss is a predeformational intrusive,and the biotite granite gneiss belongs to syndeformational intrusive.The emplacement of two granite gneiss indicates a magmatic activity event which was associated with late Achean a near WE trending tectonical deformation.
Keywords:Achean  Granite  gneiss  Predeformational  intrusive  Syndeformational  intrusive  Emplacement  and  deformation  Huadian  area  Jilin  province
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