ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
康定变质侵入岩的年代学及岩石地球化学特征
  
关键词:Kangding complex  trace elements  SHRIMP dating  magmatic arc
基金项目:本文为国家白然科学基金项目(批准号:40173007,40234052 )资助。
作者单位
李志红 国土资源部同位素地质重点实验室中国地质科学院地质研究所北京100037
中国地质大学地球与资源学院北京100083 
罗照华 中国地质大学地球与资源学院北京100083 
陈岳龙 中国地质大学地球与资源学院北京100083 
赵俊香 中国地质大学地球与资源学院北京100083 
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摘要:
Geochronological and Geochemical Characteristics of Kangding Metamorphosed Intrusions
      The Kangding metamorphosed intrusions are mainly composed of quartz diorite-tonalite -granodiorite. The ages of igneous zircons from the complex range from 721 to 773 Ma, which shows the intrusive activity during Neoproteronoic. The oldest age obtained from the intrusions is 2468 Ma, implying the involvement of materials from Yangtze craton basement. The ages of 99~531 Ma produced from zircon rims may reflect later metamorphic events. The complex shows a calc-alkaline differential trend in major elements, and the trace elements exhibit typical geochernical features of the island arc setting.
LI Zhihong,LUO Zhaohua,CHEN Yuelong,ZHAQ Junxiang.2005.Geochronological and Geochemical Characteristics of Kangding Metamorphosed Intrusions[J].Acta Geoscientica Sinica,26(z1):87-89.
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