homogenization temperature

基本解释

The fluid inclusions are of low salinity, with small gas-liquid ratio and homogenization temperature of 150-240℃.
流体包裹体气液比很小，为不饱和的低盐度包裹体。均一温度为150—240℃。
Systematical study has been carried out on thermobarogeochemical features of inclusions, and homogenization temperature, salinity and pressure were obtained.
研究了包裹体的温压地球化学特征，获得了包裹体的均一温度、盐度和压力。
The reliability of the homogenization temperature and the veracity of burial thermal evolution history is the key question in the study of infilling history of gas reser.
利用流体包裹体研究油气充注史的核心问题是流体包裹体均一化温度的可靠性、埋藏热演化史的准确性。

均一温度
Detailed study on fluid inclusions indicated that the homogenization temperature and salinity of the ore-forming fluids declined from the early to late mineralization stage, and the mineralization occurred under the low-medium pressure and epithermal conditions.
研究认为,由早期成矿阶段至晚期成矿阶段,成矿流体的均一温度和盐度依次下降。