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首页> 外文会议>Conference on Asian Current Research on Fluid Inclusions >Homogenization temperature and its significance for primary fluid inclusion in halite formed in Chaka salt lake, Qardam basin
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Homogenization temperature and its significance for primary fluid inclusion in halite formed in Chaka salt lake, Qardam basin

机译：QARKAM盆地Chaka Salt Lake中壳盐盐盐中初级液体包裹物的均化温度及其意义

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Halite precipitation with water and air temperature was observed in detail, and homogenization temperature of fluid inclusions in halite formed in ancient and modern Chaka Salt Lake was studied. Halite precipitates mainly in August every year and largely precipitates between 13 and 15pm at one day when water temperatures reach 20°C but can seldom reach 30°C. Homogenization temperatures of fluid inclusions in halite formed in Chaka Salt Lake range from 14°C to 38°C with an average of 23.7°C. The number of inclusions appears an obvious peak value at homogenization temperatures between 18 ～ 25°C, which probably represent the water temperature in which halite mainly precipitates when water temperatures reach 20°C. Therefore, homogenization temperatures of fluid inclusions in halite formed in Chaka Salt Lake can well reflect the water temperature.
机译：详细观察到与水和空气温度的盐水和空气温度，研究了古代和现代Chaka盐湖中形成的菌液中的流体夹杂物的均化温度。 宿港主要在8月份沉淀，每年八月份，当水温达到20°C时，在一天内沉淀到13至15点之间，但很少达到30°C。 在脉盐湖中形成的卤石中的流体夹杂物的均质化温度范围为14℃至38℃，平均为23.7℃。 夹杂物的数量出现在18〜25℃之间的均质温度下的明显峰值，这可能代表水温，当水温达到20°C时，留点主要沉淀的水温。 因此，在Chaka Salt Lake中形成的菌液中的均化温度均匀地反映水温。

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