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Zircon U-Pb SHRIMP ages of high-pressure granulite in Yushugou ophiolitic terrane in southern Tianshan and their tectonic implications
作者姓名:ZHOU Dingwu  SU Li  JIAN Ping  WANG Runsan  LIU Xiaoming  LU Guanxiang & WANG Juli Key Laboratory of Continental Dynamics of the Ministry of Education and
作者单位:ZHOU Dingwu,SU Li,JIAN Ping,WANG Runsan,LIU Xiaoming,LU Guanxiang & WANG Juli Key Laboratory of Continental Dynamics of the Ministry of Education and Department of Geology,Northwest University,Xi'an 710069,China Beijing SHRIMP Center,Beijing 100037,China
摘    要:Zircons from two high-pressure granulite samples from the Yushugou ophiolitic terrane, southern Tian shan have been investigated by cathodoluminescence, LA ICPMS and ion microprobe (SHRIMP) for their internal textures, trace elemental compositions and in situ dating. The weighted mean ages of these two samples are 392±7 and 390±11 Ma, respectively, representing the granulite-facies meta morphic age of the ophiolitic terrane, and indicating that the southern Tianshan ocean initiated its northward subduction since the early Devonian.

关 键 词:锆石  SHRIMP  U-Pb  年代测定  高压麻粒岩  表面形态  天山
收稿时间:2004-03-13
修稿时间:2004-04-16

Zircon U-Pb SHRIMP ages of high-pressure granulite in Yushugou ophiolitic terrane in southern Tianshan and their tectonic implications
ZHOU Dingwu,SU Li,JIAN Ping,WANG Runsan,LIU Xiaoming,LU Guanxiang & WANG Juli Key Laboratory of Continental Dynamics of the Ministry of Education and.Zircon U-Pb SHRIMP ages of high-pressure granulite in Yushugou ophiolitic terrane in southern Tianshan and their tectonic implications[J].Chinese Science Bulletin,2004,49(13):1415-1419.
Authors:Zhou  Dingwu  Su  Li  Jian  Ping  Wang  Runsan  Liu  Xiaoming  Lu  Guanxiang  Wang  Juli
Institution:(1) Key Laboratory of Continental Dynamics of the Ministry of Education and Department of Geology, Northwest University, 710069 Xi’an, China;(2) Beijing SHRIMP Center, 100037 Beijing, China
Abstract:Zircons from two high-pressure granulite samples from the Yushugou ophiolitic terrane, southern Tianshan have been investigated by cathodoluminescence, LAICPMS and ion microprobe (SHRIMP) for their internal textures, trace elemental compositions and in situ dating. The weighted mean ages of these two samples are 392 ±7 and 390 ±11 Ma, respectively, representing the granulite-facies metamorphic age of the ophiolitic terrane, and indicating that the southern Tianshan ocean initiated its northward subduction since the early Devonian.
Keywords:Yushugou ophiolite  SHRIMP U-Pb dating  granulite facies metamorphism  southern Tianshan  
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