松潘-甘孜地体内花岗岩锆石SHRIMP U-Pb定年及其构造意义

胡健民 孟庆任 石玉若 渠洪杰. 松潘-甘孜地体内花岗岩锆石SHRIMP U-Pb定年及其构造意义[J]. 岩石学报, 2005, 21(3): 867-880.
引用本文: 胡健民 孟庆任 石玉若 渠洪杰. 松潘-甘孜地体内花岗岩锆石SHRIMP U-Pb定年及其构造意义[J]. 岩石学报, 2005, 21(3): 867-880.
HU JianMin,MENG QingRen,SHI YuRuo and QU HongJie Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China Beijing SHRIMP Center,Beijing 100037. SHRIMP U-Pb dating of zircons from granitoid bodies in the Songpan-Ganzi terrane and its implications[J]. Acta Petrologica Sinica, 2005, 21(3): 867-880.
Citation: HU JianMin,MENG QingRen,SHI YuRuo and QU HongJie Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China Beijing SHRIMP Center,Beijing 100037. SHRIMP U-Pb dating of zircons from granitoid bodies in the Songpan-Ganzi terrane and its implications[J]. Acta Petrologica Sinica, 2005, 21(3): 867-880.

松潘-甘孜地体内花岗岩锆石SHRIMP U-Pb定年及其构造意义

  • 基金项目:

    国家自然科学基金项目(40272097)中国科学院知识创新项目(KZCX2-XW-119)中国地质调查局项目1212010510109资助成果

  • 松潘-甘孜地体总体上是一个三角状褶皱带,其北侧、东南侧及东侧分别与东昆仑-西秦岭构造带、金沙江构造带及龙门山构造带相邻。地体内几乎全部被三叠系浊积岩所覆盖,其中侵位了很多花岗岩体。显然,这些花岗岩的岩浆特征、来源与侵位时代,对研究松潘-甘孜地体基底性质、构造演化等问题具有重要意义。本文报道利用SHRIMP定年技术对一些花岗岩岩体锆石所进行的精确测年数据。测试结果表明:(1)松潘-甘孜地体内的花岗岩体主要形成于晚三叠世,但岩浆活动可延续到早侏罗世晚期;(2)早期花岗岩浆活动与三叠纪系褶皱变形大致同期,指示这一时期的花岗岩浆的形成可能与三叠系下部大型拆离滑脱构造相关;(3)花岗岩结晶锆石普遍具有浑圆状或不规则状较老的继承锆石核,这些核部继承锆石可能代表花岗岩浆在上升过程中从不同地层内捕获的碎屑锆石,或者是下地壳岩石深熔残留锆石。根据SHRING U-Pb定年,这些继承锆石的年龄分别为二叠纪、加里东期、晚元古代和早元古代。元古代碎屑锆石的存在也可能指示松潘-甘孜地体具前寒武系基底。
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修回日期:  2004-12-06
刊出日期:  2005-05-31

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