鲁斯矿体约含V_3O_81800吨,围岩是始新世沃萨奇砂层。在大部分砂岩中沿氧化还原前沿区可发现矿化作用。前沿是砂岩中二次氧化和初次还原的边界。铀随着地下水流过砂岩并在地球化学作用下还原沉淀下来。鲁斯矿体呈典型的卷舌状,赋存于深度120～170米厚20米的砂岩中。砂岩是自流蓄水层,渗透性为250～300毫达西。矿物主要 Ruth ore body contains about V_3O_81800 tons, the surrounding rock is Eocene Wasatch sand. Mineralization can be found along most of the sandstone along the redox frontier. The frontier is the boundary between secondary oxidation and primary reduction in sandstone. Uranium passes through the sandstone as groundwater flows and is reduced and precipitated by geochemical processes. The Ruth ore body is a typical voluptuous tongue and occurs in sandstone with depth of 120-170 meters and 20 meters. Sandstone is a gravity aquifer with a permeability of 250 to 300 millidarcies. Minerals are main