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鄂尔多斯盆地南部直罗组砂岩的孔渗性特征及其控制因素
引用本文:贾立城,;张子敏,;肖新建.鄂尔多斯盆地南部直罗组砂岩的孔渗性特征及其控制因素[J].国外铀金地质,2009(3):134-140.
作者姓名:贾立城  ;张子敏  ;肖新建
作者单位:[1]核工业北京地质研究院,北京100029; [2]中广核铀业发展有限公司,北京100081
摘    要:鄂尔多斯盆地南部中侏罗统直罗组的铀成矿条件与盆地北部相似,有形成富大砂岩铀矿的可能性.但较低的渗透性却成为制约盆地南部某些地区成矿的不利因素。分析了研究区内直罗组砂体的物性变化规律,深入讨论了成岩作用对该区直罗组砂岩物性起控制作用,为下一步铀成矿预测提供依据。

关 键 词:直罗组  砂岩物性  成岩作用

Permeability and its controlling factors of sandstone in Zhiluo Formation in the southern part of Ordos Basin
Institution:JIA Li-cheng, ZHANG Zi-min, XIAO Xin-jian (I. Beijing Research Institute of Uranium Geology, Beijing 100029, China; 2. Uranium Resources Co., Ltd, CGNPC, Beijing 100081, China)
Abstract:The metallogenic conditions for sandstone-type uranium deposits in Zhiluo Formation, Middle Jurassic in the southern part of Ordos Basin are similar to those in the northern part of the basin and consequently it is possible to form large and high-grade uranium deposits. But the permeability of main sand bodies is relatively low which restrains the uranium mineralization in the south area. Based on analyzing the spatial change of physical properties of sand bodies in Zhiluo Formation, the control of diagnesis on physical properties of sandstone has been discussed in the paper, providing a foundation for further prognosis of uranium mineralization in this area.
Keywords:Zhiluo Formation  physical properties of sandstone  diagenesis
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