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地球学报  2008 

鄂尔多斯盆地南部店头地区直罗组砂岩成岩演化与铀成矿

DOI: 10.3975/cagsb.2008.02.08

Keywords: 成岩演化,砂岩型铀矿,店头地区,鄂尔多斯盆地

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Abstract:

通过鄂尔多斯盆地南部店头地区含矿砂岩的普通薄片观察、薄片染色、阴极发光、扫描电镜及能谱分析、电子探针、全岩及粘土矿物X衍射、流体包裹体等分析,对研究区直罗组含矿砂岩成岩作用进行了较全面的研究,探讨了成岩演化与铀成矿的关系。研究认为,直罗组砂岩成岩环境经历了由酸性到碱性再到酸性、由同生期氧化→浅埋期弱还原→短暂抬升期弱氧化→深埋期还原增强→大幅度抬升期氧化还原过渡的演化过程,该过程控制着铀离子的迁移、聚集以及最终的定位。该砂岩型铀矿形成于盆地埋藏成岩作用晚期(相当于表生作用阶段)相对埋藏较浅的氧化一还原过渡带。

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