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四川汉源平等澄江期A型花岗岩地球化学特征

THE GEOCHEMICAL CHARACTERISTICS OF A-TYPE GRANITE OF CHENGJIANG PERIOD IN PINGJIANG, HANYUAN,SICHUAN PROVINCE

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【作者】 段志明李勇白宪洲黎兵

【Author】 DUAN Zhi-ming,LI Yong,BAI Xian-zhou,LI Bing Chengdu University of Technology,Chengdu 610059,China

【机构】 成都理工大学成都理工大学 四川成都610059四川成都610059四川成都610059

【摘要】 根据花岗岩同源岩浆演化系列 ,将汉源平等复式花岗岩体划分为 6个单元 ,归并为一个超单元。岩石类型以二长花岗石、钾长花岗岩为主体 ,具明显的成分—结构演化特征。岩石化学以富硅、钾 ,贫钙 ,岩石稀土以具明显的铕负异常为特征。本超单元同位素年龄为 6 5 0 Ma~ 70 0 Ma,它是澄江期非造山带 ,沿火山裂谷侵位的 A型花岗岩。

【Abstract】 According to the theory of the consanguinity of magma and the evolution order,the multiple granite in Pingdeng can be devided into six units,whic incorporated into a super-unit. The rock type mainly includes adamanite,moyite which have distinct features of texture and composition respectively.The petrochemistry is characterized by rich-silicon,rich-potassium,poorcalcium,and appearant loss of Eu element.The isotopic age of the supper-unit is between 650 Ma to 700 Ma.The rock is A-type granite,which invaded volcano rift in anorogenic Chengjiang Period.

  • 【文献出处】 矿物岩石 ,Journal of Mineralogy and Petrology , 编辑部邮箱 ,2003年02期
  • 【分类号】P588.121
  • 【被引频次】1
  • 【下载频次】140
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