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新疆尉犁县风屏北山片麻杂岩地质特征及原岩成因探讨
引用本文:刘延军,时玉芹,王伯勋,郑鹤龄,姚建民.新疆尉犁县风屏北山片麻杂岩地质特征及原岩成因探讨[J].吉林地质,2009,28(1):18-22.
作者姓名:刘延军  时玉芹  王伯勋  郑鹤龄  姚建民
作者单位:吉林省第三地质调查所,吉林,四平,136000
摘    要:对风屏北山片麻杂岩进行了同位素年龄确定,采用SHR IMP放射性同位素测年,确定同位素定年结果为2 484±20 Ma。根据岩石化学、稀土、微量元素等特征,对片麻杂岩进行了分析研究,认为该片麻岩原岩为I型花岗岩,经区域变质作用形成。

关 键 词:片麻杂岩  原岩恢复  I型花岗岩  原岩成因

Geological features of the northern Fengpingshan gneiss complex and protolith genesis of Weili County,Xinjiang
LIU Yan-jun,SHI Yu-qin,WANG Bo-xun,ZHENG He-ling,YAO Jian-min.Geological features of the northern Fengpingshan gneiss complex and protolith genesis of Weili County,Xinjiang[J].Jilin Geology,2009,28(1):18-22.
Authors:LIU Yan-jun  SHI Yu-qin  WANG Bo-xun  ZHENG He-ling  YAO Jian-min
Institution:( The Third Geologic Survey of Jilin Province, Siping 136000, Jilin, China)
Abstract:The isotopic age of the northern Fengpingshan gneiss complex was determined using SHRIMP radioactive isotope dating, the result shows that isotopic age is 2 484±20 Ma. The gneiss complex was analyzed on the basis of the petrochemistry, RE and microelement characteristics. It is considered that gneiss complex belongs toⅠ type granite through the regional metamorphism.
Keywords:gneiss complex  protolith reconstruction  Ⅰ type granite  protolith genesis
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