问题的提出某些后生层状矿化的形成与含氧层间水同上升还原溶液的相互作用有关。许多人在解释断裂带附近铀矿石的生成条件时采用了类似的溶液相互作用模式。这些矿石常常叠加在层间氧化带的或原生红化的透水岩石上,并具有独特的赤铁矿-沥青铀矿型矿物组合;同时,在微 The question raised some of the epigenetic stratiform mineralization and the formation of oxygen-containing layer of water with the rise of the interaction between the reduction solution. Many people used similar solution interaction modes to explain the conditions for uranium ore formation near the fault zone. These ores are often superimposed on interlayer oxidized or primary redified water-permeable rocks and have a unique hematite-bitumen type mineral assemblage. At the same time,