新疆伊犁盆地南缘新生代构造特征及其对砂岩型铀矿的控制作用  

THE STRUCTURE CHARACTERISTIC OF CAINOZOIC ERA TO CONTROLSANDSTONE URANIUM ACTION IN SOUTH YILI BASIN IN XINJIANG

作　　者：李宝新 徐建国 王冰 刘陶勇 

机构地区：[1]中国核工业地质局216大队,新疆乌鲁木齐830011

出　　处：《新疆地质》2008年第3期297-300,共4页Xinjiang Geology

摘　　要：通过对伊犁盆地南缘新生代构造运动发生期次、时间的研究,阐明了盆地构造发育特征,并进一步阐述盆地南缘新构造运动对砂岩型铀矿形成的控制作用,探讨它们之间的关系,为进一步的找矿工作奠定了基础.Based on a study of the periods and time of the tectonic movement occurs to the southern margin of Yili Basin in Cainozoic ,this paper expounded the characteristics of the tectonics developed in the basin,further elaborated the control function of the tectonic movement in Cainozoic to the sandstone uranium mine formation in the southern margin of Yili Basin and discusses the relations of them, thus instruct the next step prospecting work.

关 键 词：伊犁盆地南缘 新生代构造运动 砂岩型铀矿 控制作用 

分 类 号：P619.14[天文地球—矿床学]