均一温度

均一温度为90～130°C时出现低成熟度油田；

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

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。

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

在均一温度<300℃时，CO2NaClH2O流体的盐度低于盐水溶液的盐度，前者的压力均值高于后者。

When the homogenization temperatures are lower than 300 ℃, the salinity of CO_2-NaCl-H_2O fluid is lower than that of NaCl-H_2O fluid .

然而，不含矿的脉石英所含流体包裹体的均一温度仅限于145～175℃，盐度10.2%～12.9%，不含CO2气、液包裹体。

However , the homogenization temperature of fluid inclusions in the non-mineralized quartz veins range from 145 to 175 ℃ and their salinity change from 10.2 % to 12.9 % with no gas phase or liquid phase CO_2 inclusions .

根据大坪石墨的拉曼光谱D：O峰强度比，估计这些石墨形成于麻粒岩相变质温度条件下，与石英中富CO2流体包裹体的均一温度（300.0~420.0℃）极不相称；

Based on D ∶ O peak intensity ratios , these graphite inclusions formed at granulite-facies metamorphic temperature , which is much higher than the homogeneous temperature ( 300.0 ~ 420.0 ℃) of the CO_2-enriched fluid inclusions in the graphite-bearing quartzes .

第一期包裹体为主含CO2、N2和H2O成分的油气包裹体，均一温度相对较低，主峰为120℃，代表了早期天然气初次形成、运移和成藏事件。

Organic compositions of the first phase of inclusions Mainly consis of CO2 , N2 and H2O , homogenization temperatures are relatively low , the main peak is 120 ℃, which represents the early gas formation , migration and accumulation event .

气烟囱、沸腾包裹体、MnO等微量元素与包裹体均一温度异常等是判断或追踪断裂带流体活动特征的有效指标。

Whereas gas chimneys , boiling fluid inclusions , MnO trace elements and the abnormal temperature of fluid inclusions are all the characteristics for determining or tracking the migration of fluid inclusions in fault zones .

热液为低盐度流体，其成分主要为H2O，含少量CO2，其总体密度为0.79~0.95g/cm3。包裹体均一温度变化范围大，为134.7~269.5℃。

The hydrothermal liquid is of low sanity , and the component mainly is H 2O with little CO 2 , and the general density is 0.79 ~ 0.95 g / cm 3 . The homogenous temperature varies greatly , i.e. , 134.7 ~ 269.5 ℃ .

根据断层岩中发育的包裹体的均一温度、断层带中方解石脉的碳氧同位素测定结果，确定了该断层的最小贯穿深度为6500m，至少断至侏罗系的烃源岩。

The measured homogeneous temperatures of inclusions in fault rock and C and O isotope values in calcite vein demonstrate that the fault extents downward to a depth of 6500 meters at least .

根据裂缝交切关系、方解石包裹体均一温度和岩石Kaiser实验结果，认为O2+3灰岩遭受3次构造运动，形成了相应的3期构造裂缝。

It is believed that , on the basis of intersected relations of the rift and testing results of homogeneous temperature of calcite packet and rock Kaiser , O 2 + 3 limestone had gone through three times of tectonic movements , forming corresponding 3 phases of structural rifts .

流体包裹体测定，均一温度为105℃-178℃。

Flow inclusion measured range between 105 and 178 celsius degrees .

盐水包裹体的均一温度为80～170℃。

The homogenization temperatures of aqueous inclusions are 80 ~ 170 ℃ .

均一温度直方图分为连续分布型和非连续分布型两类：前者表示连续性的充注一期成藏；

The continuous distribution type indicates continuous charging and just one-period accumulation .

熔融包裹体均一温度及挥发组分含量测试

Tests of Homogenization Temperature and Volatile Content of Melt Inclusions

熔融包裹体的均一温度为925℃。

Thehomogenization temperature of the melt inclusions is925 ℃ .

均一温度系统的热爆炸和起爆延滞期

Thermal explosion and times-to-ignition in uniform - temperature systems

流体包裹体均一温度显示成矿流体为中低温热液。

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

流体包裹体均一温度为181～267℃；

Homogenization temperatures are from 181 to 267 ℃ .

结垢包裹体的均一温度为102-120℃，反映了结垢的形成温度。

The average temperature of inclusions is about 102-120 ℃ which shows the scaling temperature .

流体包裹体的均一温度高异常是由热流体活动所导致的。

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

包裹体粒度较小时，其均一温度往往都要低一些；

It is generally easier for a smaller inclusion to be homogenized at a relatively lower temperature .

矿床包裹体发育，类型复杂，均一温度在180～300℃之间。

Homogenous temperature of fluid inclusion in quartz for the deposit varies from 180 to 300 ℃ .

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 fluid inclusions are of low salinity , with small gas-liquid ratio and homogenization temperature of 150-240 ℃ .

包裹体均一温度在135℃～290℃之间，与辉锑矿形成温度相吻合；

The homogeneous temperature of inclusions is between 135 ℃~ 290 ℃, according to the forming temperature of stibnite .

成矿均一温度为160～270℃。

The homogeneous temperature of quartz fluid inclusion is in the range of from 160 ℃ to 270 ℃ .

均一温度为266.5～295.2℃，属中温热液矿床。

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

在推覆体内部，从推覆体前锋到主滑面流体的均一温度逐渐降低。

The homogeneous temperature in the nappe decreased gradually from the nappe front to the fault surface underlying the nappe .

显微温度测试必须以油气包裹体鉴定为基础，单纯应用均一温度划分油气运移期次是不合适的。

It is not appropriate to classify the stages of petroleum migration only by applying homogenization temperatures of various inclusions .

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。

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

均一温度为190～340℃与370～410℃；

The temperatures of total homogenization ranged from 190 C to 340 C , and from 370 C to 410 C.