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粤北下庄花岗岩锆石U-Pb年龄及Hf同位素特征
陈佑纬;  毕献武;  胡瑞忠;  戚华文;  齐有强;  胥磊落
2009
Conference Name中国矿物岩石地球化学学会第12届学术年会
Source Publication中国矿物岩石地球化学学会第12届学术年会
Issue1
Conference Date2009-04
Conference Place中国贵州贵阳
Abstract

下庄岩体位于粤北贵东岩体的东部,是贵东岩体主要的赋铀及产铀花岗岩体,出露面积约157km~2。以往认为为燕山期花岗岩。近年来的研究表明它是印支期花岗岩。由于技术条件的限制,前人判断为壳源岩。本文以原位Hf同位素比值分析,

Language中文
Document Type会议论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/7839
Collection中国科学院地球化学研究所
矿床地球化学国家重点实验室
Recommended Citation
GB/T 7714
陈佑纬;毕献武;胡瑞忠;戚华文;齐有强;胥磊落. 粤北下庄花岗岩锆石U-Pb年龄及Hf同位素特征[C],2009.
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