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中天山早泥盆世陆弧:来自花岗质糜棱岩地球化学及SHRIMP-U/Pb定年的证据
引用本文:杨天南,李锦轶,孙桂华,王彦斌.中天山早泥盆世陆弧:来自花岗质糜棱岩地球化学及SHRIMP-U/Pb定年的证据[J].岩石学报,2006,22(1):41-48.
作者姓名:杨天南  李锦轶  孙桂华  王彦斌
作者单位:中国地质科学院地质研究所,北京,100037
摘    要:中天山巴伦台以北地区出露一套糜棱岩化的中-酸性侵入岩,元素地球化学特点表明其属于火山弧环境;锆石SHRIMP U/Pb法测试结果揭示其侵位年龄在405—416Ma间,属早泥盆世。这一研究结果显示,早在晚志留世晚期,南天山洋已开始向北俯冲,并在中天山地块南缘形成火山弧环境。至早泥盆世晚期,塔里木陆块与中天山火山弧发生碰撞。

关 键 词:糜棱岩化花岗岩  地球化学  SHRIMP锆石U-Pb年龄  中天山
文章编号:1000-0569/2006/022(01)-0041-48
收稿时间:11 11 2005 12:00AM
修稿时间:12 5 2005 12:00AM

Earlier Devonian active continental arc in Central Tianshan:evidence of geochemical analyses and Zircon SHRIMP dating on mylonitized granitic rock.
YANG TianNan,LI JinYi,SUN GuiHu,WANG YanBin.Earlier Devonian active continental arc in Central Tianshan:evidence of geochemical analyses and Zircon SHRIMP dating on mylonitized granitic rock.[J].Acta Petrologica Sinica,2006,22(1):41-48.
Authors:YANG TianNan  LI JinYi  SUN GuiHu  WANG YanBin
Institution:Institute of Geology, Chinese Academy of Geological Science, Beijing 100037, China
Abstract:Mylonitized dioritic-granitic plutons occurred in north of Baluntai area,central Tianshan,Northwest China.Element geochemical data reveal that the dioritic-granitic plutons were generated at active continental arc environment like today's Chile;zircon U/Pb SHRIMP dating and CL imaging indicat that the active continental volcano arc developed at 405 -416 Ma.These data demonstrat that the paleo-south Tianshan ocean crust started northward subducting under the central Tianshan block at earlier Devonian,resulting in a continental arc upon the overriding plate.The following collision between the central Tianshan block and the Tarim block might begin at later of Earlier Devonian.
Keywords:Mylonitized dioritic-granitic pluton  geochemistry  zircon U/Pb SHRIMP dating  central Tianshan  
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