中文摘要：

笔者对相山铀矿田邹家山矿床铀矿石中的流体包裹体进行研究，结果表明该矿床的均一温度分布范围较广，为122-360℃。矿床形成温度有两个阶段，分别是高温阶段213-360℃（平均值为263．1℃）和低温阶段122-185℃（平均值为142．7℃），属于中低温热液铀矿床。高温阶段盐度变化范围为（1．74～7．31）wt％（平均值为3．77wt％），低温阶段盐度变化范围为（0．88～2．57）wt％（平均值为1．64Wt％）。矿床成矿溶液高温段的平均密度0．78g／cm3，成矿压力204．57×10^5Pa，成矿深度0．68km；低温段的平均密度0．92g／cm3，成矿压力96．08×10^5Pa，成矿深度0．32km。据此推测，邹家山铀矿床的成矿流体来源主要是岩浆期后热液，同时伴有大气水热液。

英文摘要：

This paper is mainly on the fluid inclusions of uranium ores form Zoujianshan deposit in Xiangshang uranium ore-field. Test result of fluid inclusions shew that the homogenization temperature distributed in a wide range from 122℃ to 360 ~C and can be divided into two phases. The high temperature phase was from 213 to 360℃ with the average of 263. 1℃ and low temperature phase was from 122 to 185℃ with the average of 142.7℃, which suggest that the deposit falls into median-low temperature hydrothermal deposits. In high temperature phase, the salinity of inclusion was （1.74-7.31） wt% with the average value of 3.77wt%, and in low temperature phase the salinity ranged from 0.88wt% to 2.57wt% with the average of 1.64wt%. In high temperature phase, the mineralization solution was with the average density of 0. 78g/cm3 and the pressure of 204. 57 × 10^5 Pa which refer to the depth of 0.68km. In low temperature phase the mineralization solution was with the average density of 0.92g/cm3 and pres- sure of 96.08×10^5Pa which refer to the depth 0. 32kin. By summarizing the above information, we can inferred that the ore forming fluid is the main from post-magmatic hydrothermal fluid which was accom- panied by atmospheric water.