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曾经用原子吸收、比色法、中子活化等方法分析拉比特湖铀矿床中自形石英、自云石包果体中组成盐水的离子比例。这些盐水基本上都是成矿溶液,来自阿萨巴斯卡砂岩,由于盐水与基底围岩反应而发生变化。拉比特湖铀矿床位于阿萨巴斯卡砂岩盆地的东部,以前曾对此矿床作过详细描述。尼平(H.D.Knipping)曾发表了拉比特湖石英和白云石气液包果体做为微温度计的研究结果。石英由于含CO_2和碳氢化合物的盐水(相当于30%NaCl 重量)溶液,是在160℃及700巴压条件下形成的。晚期的白云石是含不可溶的CO。气泡的盐水(相当于28%NaCl 重量)溶液,在较低的温度(但不低于130℃)条件下形成的。
Atomic absorption, colorimetry, neutron activation and other methods have been used to analyze the proportion of self-shaped quartz in the La Bitite lake uranium deposit, and the proportion of ions that make up the saltwater in the magma. These are basically mineralized solutions, from the Athabasca sandstone, which change as the brine reacts with the surrounding rock. The labitite lake uranium deposit is located east of the Athabasca sandstone basin, which was previously described in detail. H.D.Knipping published the results of a study on the microthermometer of the bagged quartzite and dolomite gas reservoir in Lake Rabbit. Quartz is formed at a temperature of 160 ° C and a pressure of 700 bar due to a solution of CO 2 and hydrocarbon-containing brine (corresponding to 30% by weight of NaCl). Late dolomite is insoluble in CO. Bubble saline solution (equivalent to 28% NaCl weight) is formed at a lower temperature (but not lower than 130 ° C).