homogenization temperature

Thermal fluid activity results in higher abnormality of homogenization temperature of fluid inclusions too .

流体包裹体的均一温度高异常是由热流体活动所导致的。

There appears lower matured oil field when the homogenization temperature of fluid inclusions is 90 to 130 ° C ;

均一温度为90～130°C时出现低成熟度油田；

Tests of Homogenization Temperature and Volatile Content of Melt Inclusions

熔融包裹体均一温度及挥发组分含量测试

Homogenization temperature indicates that ore-forming fluid is low to moderate temperature hydrothermal .

流体包裹体均一温度显示成矿流体为中低温热液。

Effect of Homogenization Temperature and Hot Rolling Pass on Morphology of Compound in 3104 Sheet

均匀化温度、热轧道次对3104制罐板化合物形貌的影响

A new method for estimating the removed thickness of sediment using homogenization temperature of fluid inclusions

恢复地层剥蚀厚度的一种新方法&包裹体测温法

The data on the inclusion homogenization temperature show that the oil and gas reservoirs were formed in Late Mesozoic-Cenozoic .

包裹体均一化温度反映油气成藏期位于中生代晚期&新生代。

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℃。

Measurement and Geologic Application of Homogenization Temperature and Salinity of Inclusions in Authigenic Quartz of Sandstone

砂岩中自生石英包裹体均&温度和盐度测定及地质应用

Using fluid inclusion homogenization temperature and analog inclusion pressure , dissolving capacity of methane in water can be confirmed .

利用包裹体的均一温度和模拟的包裹体压力，确定了水对甲烷的溶解能力。

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400℃以下均匀化，合金硬度降低，电导率则升高；

Natural gas composition and isotope characteristics could trace gas migration direction . Accumulation periods are divided using homogenization temperature of inclusion and other elements .

通过天然气组分及同位素特征示踪天然气运移方向，利用包裹体及其他成藏条件演化判定成藏期次。

Furthermore , the homogenization temperature obtained from inclusion fluid was between 58 ℃ and 176 ℃ with an average temperature of 114.9 ℃ .

矿石流体包裹体均一温度为58～176℃，平均114.9℃。

The homogenization temperature of fluid inclusions ranges from 266.5 ℃ to 295.2 ℃, belonging to the mesothermal type .

均一温度为266.5～295.2℃，属中温热液矿床。

Higher homogenization temperature display deep copper mineralization may not belong to the epithermal-type and reflect mineralization may be directly related to magmatic .

较高的均一温度显示深部铜矿体成矿作用可能不是属于浅成低温热液型，可能为中高温热液型，反映成矿可能与深部岩体直接相关。

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。

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。

According to the homogenization temperature , we can find out that the oil and gas in this area are in maturation-high maturation evolution stage .

根据包裹体均一温度可知，本区油气为高成熟阶段。

The statistics of homogenization temperature and salinity of oil inclusion and saline inclusion indicates that the second and third hydrothermal fluids are dominating .

油包裹体和盐水包裹体均一温度以及盐水包裹体盐度的统计结果表明，第2期和第3期热流体活动占主导地位。

The sulfur isotopes balance temperature of galena and sphalerite is 214 ℃ which is close to the homogenization temperature of fluid inclusions .

方铅矿和闪锌矿中S同位素平衡温度计算结果为214℃，与包裹体测温结果相近。

Characteristics of organic inclusions and their homogenization temperature were studied . The relationship between vitrinite reflectance ( R o ) and history of geological evolution was analyzed .

研究了有机包裹体及其均一温度的特征，分析了镜质组反射率（Ro）与地质演化史的关系。

Besides microscopic analysis of fluid inclusions , measurement and analysis of the homogenization temperature and the melt temperature have been carried out for times and stages analysis of hydrocarbon accumulation history .

镜下观察流体包裹体，并对与烃类共生的盐水包裹体进行均一化温度和冰融点测试，进行油气藏成藏期的分析。

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。

Compared with the former , the inclusion in the latter was characterized by its complex assemblage in types , and higher homogenization temperature , salinity and trapped pressure .

前者的包裹体类型简单，均一温度、盐度和捕获压力较低.后者以包裹体类型复杂、均一温度及捕获压力较高为特征。

Through the analysis of stable carbon and oxygen isotopes of calcite veins and homogenization temperature of fluid inclusion , the ancient meteoric water infiltration depth was recovered .

通过方解石脉稳定碳氧同位素和包裹体均一温度测定，恢复了黔南桂中坳陷海相地层古大气水下渗深度。

Macroscopic and microscopic geological characteristics of this mineral deposit are described and the properties of metallogenetic fluid are discussed by using the test results of homogenization temperature and composition of inclusion .

描述了三类矿床宏观与微观地质特征；运用包裹体均&温度和包裹体成分测试成果探讨了成矿流体性质；

The hydrocarbon migration stages and accumulation in Karamay oilfield , Junggar Basin , can be discussed by using geochemical information of crude oil and homogenization temperature of fluid inclusions .

根据原油地球化学特征以及流体包裹体均一温度，探讨了准噶尔盆地克拉玛依油田油气运聚期次及成藏特征。

Deals with the form , size , gas / liquid ratio , explosion and homogenization temperature , and salinity of the inclusions of minerals in main type antimony deposits in China .

讨论了中国主要类型锑矿床矿物包裹体形态、大小、气液比值、包裹体爆裂温度、均一化温度和盐度。

The inclusion homogenization temperature measurement and salinity determination lead to division of the formation process of the reservoir into 3 stages , which is consistent with the result the microscopy observations .

根据包裹体均一温度和盐度的测试结果，可以将油气的成藏期次大致划分为3期，与显微观察研究认识一致。

Characteristics of hydrocarbon accumulation in typical oil and gas fields in the northern edge of Qaidam basin are analyzed by using homogenization temperature and compositions of inclusions and trap evolution history .

运用包裹体均一化温度、包裹体成分以及圈闭演化历史分析等研究方法，对柴北缘典型油气田油气成藏特征进行了分析。