吉林南部通化地区古元古代辽吉花岗岩的侵位年代与形成构造背景

路孝平 吴福元 张艳斌 赵成弼 郭春丽. 吉林南部通化地区古元古代辽吉花岗岩的侵位年代与形成构造背景[J]. 岩石学报, 2004, 20(3): 381-392.
引用本文: 路孝平 吴福元 张艳斌 赵成弼 郭春丽. 吉林南部通化地区古元古代辽吉花岗岩的侵位年代与形成构造背景[J]. 岩石学报, 2004, 20(3): 381-392.
LU XiaoPing,WU FuYua,ZHANG YanBin,ZHA0 ChengBi,GU0 ChunLi College of Earth Scicnces,Jilin University,Changchun 130061,China Rngional Geological and Mineral Resources Survey of Jilin Province,Changchun 130062,China Institute of Geology and Geophysics,Chinese Academy of Scicnces,Beijing 100029,China. Emplacement age and tectonic setting of the Paleoproterozoic Liaoji granites in Tonghua area, southern Jilin province[J]. Acta Petrologica Sinica, 2004, 20(3): 381-392.
Citation: LU XiaoPing,WU FuYua,ZHANG YanBin,ZHA0 ChengBi,GU0 ChunLi College of Earth Scicnces,Jilin University,Changchun 130061,China Rngional Geological and Mineral Resources Survey of Jilin Province,Changchun 130062,China Institute of Geology and Geophysics,Chinese Academy of Scicnces,Beijing 100029,China. Emplacement age and tectonic setting of the Paleoproterozoic Liaoji granites in Tonghua area, southern Jilin province[J]. Acta Petrologica Sinica, 2004, 20(3): 381-392.

吉林南部通化地区古元古代辽吉花岗岩的侵位年代与形成构造背景

  • 基金项目:

    国家自然科学基金(40272045),中国科学院“百人计划”资助

  • 辽吉南部古元古代花岗岩极为发育,其中最著名的是具有条痕状构造的正长花岗岩,俗称辽吉花岗岩。因该花岗岩具有条带状、条痕状和似层状构造特征,而被前人认为是由太古宙或元古宙沉积地层经变质变形作用形成,或是交代成因的混合岩。本文通过对分布于吉林南部通化地区辽吉花岗岩的典型代表一钱桌沟岩体的详实野外地质填图及地球化学研究,确定该岩体属岩浆成因的“A”型花岗岩,其岩浆侵位年龄为2160Ma左右。结合目前获得的该区古元古代地层的碎屑锆石年龄,本文认为辽吉花岗岩是辽吉地区古元古代地层沉积的基底岩石,是地层沉积之前地壳拉张作用的结果,属于一种非造山型花岗岩。
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修回日期:  2003-04-23
刊出日期:  2004-05-31

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