首页 | 本学科首页   官方微博 | 高级检索  
     检索      

贵东岩体地质地球化学特征及其形成的构造环境识别
引用本文:李建红,卫三元,梁良,冯明月.贵东岩体地质地球化学特征及其形成的构造环境识别[J].铀矿地质,2004,20(6):321-329.
作者姓名:李建红  卫三元  梁良  冯明月
作者单位:1. 核工业北京地质研究院,北京,100029
2. 东华理工学院,江西,抚州,344000
摘    要:本文在研究贵东花岗岩岩体岩石矿物组合、结构构造等地质特征的基础上 ,运用花岗岩的岩石化学、微量元素和同位素等分析数据 ,采用目前广泛应用的几种岩石化学图解、微量元素和同位素图解等方法 ,判别了贵东岩体形成的构造环境为造山带后碰撞型

关 键 词:贵东岩体  地质地球化学  构造环境
文章编号:1000-0658(2004)06-0321-09
修稿时间:2004年6月11日

Geologic-geochemical characteristics of Guidong granitic massif and recognition of geo-tectonic environment at the time of its emplacement
LI Jian-hong ,WEI Shan-yuan ,LIANG Liang ,FONG Ming-yue.Geologic-geochemical characteristics of Guidong granitic massif and recognition of geo-tectonic environment at the time of its emplacement[J].Uranium Geology,2004,20(6):321-329.
Authors:LI Jian-hong  WEI Shan-yuan  LIANG Liang  FONG Ming-yue
Institution:LI Jian-hong 1,WEI Shan-yuan 1,LIANG Liang 2,FONG Ming-yue
Abstract:Based on the study of geologic characteristics,such as mineralogic assembladge,structural and textural features of granite of Guidong granitic massif,and by using petrochemical,trace-element and isotopic data,and some petrochemical,trace-element and isotopic diagrams widely applied to the identification of geo-tectonic environments,authors recognize that Guidong granitic massif was emplaced in post-orogenic collision environment.
Keywords:Guidong granitic massif  geology-geochemistry  geotectonic environment
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号