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在普查热液铀矿床时,研究岩石裂隙渗透性是很重要的,因为它是分散晕和成矿作用的决定性因素。对现代火山作用的观察证明,热液大部分是通过裂隙渗透性较高的地带而排出的。岩石的强烈热液改造作用发生在裂隙连通的有广泛水动力相互作用的地区。而在普查热
It is important to study rock fracture permeability in the census of hydrothermal uranium deposits because it is a decisive factor in dispersion and mineralization. Observation of the role of modern volcanoes has shown that most of the hydrothermal fluid is discharged through zones of high permeability. The intense hydrothermal reforming of rocks takes place in areas where there is extensive hydrodynamic interaction between fractures. In census heat