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库捷尔太铀矿床干酪根特征研究
引用本文:李满根,周文斌,张展适,施小平.库捷尔太铀矿床干酪根特征研究[J].华东地质学院学报,2002,25(3):181-186.
作者姓名:李满根  周文斌  张展适  施小平
作者单位:东华理工学院,江西抚州344000
摘    要:在研究砂岩型铀矿床时,可以发现铀与有机质之间有着密切的关系。本文以伊犁盆地库捷尔太铀矿床为例,介绍了该矿床的基本特征,研究了该矿床中干酪根的主要组分、反射率、热解色谱分析等特征。认为研究区含矿岩系中有的有机质属中间过渡型,其原始母质为陆生高等植物,为判别有机质与铀成矿之间的关系提供了重要信息。

关 键 词:有机质  铀矿床  干酪根  伊犁盆地  成矿作用  反射率  热解色谱分析
文章编号:1000-2251(2002)03-181-06
修稿时间:2002年7月15日

Kerogen Characteristics of Kujieertai Uranium Ore Deposit
LI Man-gen,ZHOU Wen-bin,ZHANG Zhan-shi,SHI Xiao-ping.Kerogen Characteristics of Kujieertai Uranium Ore Deposit[J].Journal of East China Geological Institute,2002,25(3):181-186.
Authors:LI Man-gen  ZHOU Wen-bin  ZHANG Zhan-shi  SHI Xiao-ping
Abstract:In the study of sandstone type uranium deposits, it can be found out that uranium is closely related to organic matter. This paper studies the Kujieertai Uranium Ore Deposit in Yili Basin, introduces its basic characteristics, and tries to study the main composition, the reflectance, and the chromatographic analysis. The results show that the organic matters of this deposit would be a intermediate type. The main source of organic matters would be terrestrial higher plants. The results will be advantageous to study the relationship between organic matter and uranium.
Keywords:organic matter  sandstone type uranium deposit  kerogen
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