when the homogenization temperature increases further, more equilibrium phases are dissolved and the matrix, and the conductivity of the alloy decreases.
均匀化温度愈高,平衡相溶解愈充分,合金的电导率下降愈多。
the microscopic observation and homogenization temperature determination experiment of melt inclusions in plagioclase and olivine in basalt phenocrysts from the mariana trough were made.
对马里亚纳海槽玄武巖斜长石和橄榄石斑晶中的熔融包裹体进行了镜下观察和均一化测温实验。
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 reservoirs by using fluid inclusion.
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、埋藏热演化史的準确性。
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℃。
the homogenization temperature of the organic fluid inclusions in the fissures of sandstone reservoir is 70~80℃, 90~110℃ and 120~140℃.
主要目的层砂巖裂隙中的流体包裹体形成温度主要为三个温度区间:70~80℃,90~110℃及120~140℃;
the homogenization temperature distribution of hydrocarbon inclusions shows positive correlation with the diagenesis of host minerals.
体均一温度分布与宿主矿物成巖作用具有正相关关系。
the homogenization temperature and oil and gas components of the fluid inclusion are the important content of researching oil reservoir forming time and oil and gas resource at present.
包裹体均一温度和包裹体中油气组分是目前研究油气藏成藏时间和油气源的重要内容。
the results show that when homogenization temperature is below 400 ℃, the hardness of the alloy decreases but electro conductivity increases;
实验结果表明,在40 0℃以下均匀化,合金硬度降低,电导率则升高;
on the basis of homogenization temperature of inclusion, combining with thermal evolution history of the basin, infilling time of gases reservoirs of ordos basin is analyzed.
本文将从流体包裹体均一化温度测定出发,结合盆地热演化史,系统分析鄂尔多斯盆地上古生界各个含气层系的油气充注史。
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、埋藏热演化史的準确性。
the characteristics and the homogenization temperature of the fluid inclusions in 16 wells of chengbei fault terrace zone were analyzed in dagang oilfield.
对埕北断阶区16口井的流体包裹体特征和均一温度进行了分析,埕北断阶区储层流体包裹体分为盐水包裹体和有机包裹体。
homogenization temperature and salinity of ore-forming fluid show some regularity at space, this indicates that ore-forming fluid flow has directivity.
成矿流体的均一温度和盐度在空间上都有一定的变化规律,表明成矿演化具有定向性。
the elements diffused more evenly during homogenization, as the homogenization temperature increases or the time prolongs.
在均匀化过程中,随着均匀化温度的升高和时间的延长,偏析元素逐渐扩散均匀;
the existence of boiling inclusion group and high saline inclusions with many kinds of daughter minerals, homogenization temperature 400—250℃, is the main indicator for cu (mo) ore prospecting.
提出具有一定特征包裹体的中—酸性斑巖为找矿前提;沸腾包裹体群和含多种子矿物及高盐度的包裹体发育,且均一温度为400~250℃等均为主要找矿标志和评价依据。