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砂岩型铀矿赋存于沉积盆地的砂体之中,规模和产状适中的砂体是砂岩型铀矿含矿流体运移与铀矿储存的空间(焦养泉,2005),其形成的背景、过程、后期改造及保矿过程都与盆地的演化密切相关,因此需要对盆地进行整体分析来研究砂岩型铀矿。到目前为止,国内外运用盆地分析理论进行砂岩型铀矿分析和预测的仍然较少。本文尝试从盆地整体分析的思路出发,研究
Sandstone-type uranium deposits occur in the sand bodies of the sedimentary basins, and the sand bodies of moderate size and occurrence are the space for ore-bearing fluid migration and uranium deposit in sandstone-type uranium deposits (Jiao Yangquan, 2005). The background, The process, the post-transformation and the deposit process are all closely related to the evolution of the basin. Therefore, a comprehensive analysis of the basin is needed to study sandstone-type uranium deposits. So far, the analysis and prediction of sandstone-type uranium deposits using basin analysis theory both at home and abroad are still few. This article attempts to start from the idea of the overall basin analysis, research