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阿尼玛卿蛇绿岩带花岗—英云闪长岩锆石U—Pb同位素定年及大地构造意义
引用本文:边千韬,李涤徽.阿尼玛卿蛇绿岩带花岗—英云闪长岩锆石U—Pb同位素定年及大地构造意义[J].地质科学,1999,34(4):420-426.
作者姓名:边千韬  李涤徽
作者单位:1. 中国科学院地质研究所, 北京100029;2. 中国科学院科学出版社, 北京100717
基金项目:国家自然科学基金资助项目
摘    要:对阿尼玛卿蛇绿岩带布青山段花岗—英云闪长岩进行的锆石U—Pb同位素定年及岩石化学研究表明,该岩体锆石U—Pb年龄为402±24Ma,归属加里东末期,并非二叠-三叠纪同造山岩浆活动的产物;岩石属钙碱系列,具岛弧花岗岩特征,暗示着本区在早古生代发生过洋壳俯冲及岛弧岩浆活动事件,并为本区早古生代蛇绿岩的存在提供了佐证。

关 键 词:阿尼玛卿蛇绿岩带  布青山段  花岗—英云闪长岩  加里东末期  岛弧岩浆作用
收稿时间:1999-03-05
修稿时间:1999-03-05;

ZIRCON U-Pb AGE OF GRANODIORITE-TONALITE IN THE A'NYEMAQEN OPHIOLITIC BELT AND ITS TECTONIC SIGNIFICANCE
Bian Qiantao,Luo Xiaoquan,Chen Haihong,Zhao Dasheng.ZIRCON U-Pb AGE OF GRANODIORITE-TONALITE IN THE A'NYEMAQEN OPHIOLITIC BELT AND ITS TECTONIC SIGNIFICANCE[J].Chinese Journal of Geology,1999,34(4):420-426.
Authors:Bian Qiantao  Luo Xiaoquan  Chen Haihong  Zhao Dasheng
Institution:1. Institute of Geology, Chinese Academy of Sciences, Beijing 100029;2. Science Press, Chinese Academy of Sciences, Beijing 100717
Abstract:Zircon U-Pb age determination and lithochemistry research of the granodiorite-tonalite intruded in Buqinshan ophiolitic melange,the western sector of A’nyemaqen Ophiolitic Belt, are first done and reported in this paper. Its zircon U-Pb age is 402±24Ma and belongs to Late Caledoian. The rock belongs to calc-alkaline series, has the features of island-arc granite,which hints that oceanic crust subduction and island-arc magmatism event occurred in the area in Early Paleozoic. The research achievement is of great significance to re-understand the tectonic framework and evolution of the area,even the Central Orogenic Belt.
Keywords:A'nyemaqen ophiolitic belt    Granodiorite\|tonalite    Late Caledonian  Island\|arc magmatism
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