| 1. | Homogenization temperatures of fluids inclusions in quartz studied are above 200
所研究的石英中包裹体的均一温度高于200 。 |
| 2. | Based on the homogenization temperature of inclusive , confirm two migrating periods existing
根据包裹体均一温度确定了油气主要运移时期有二期。 |
| 3. | The coi - rich " inclusions and normal nacl + h2o inclusions are commonly observed in same samples with the same homogenization temperature ( th ) . 4
Ar - ar同位素地球化学研究表明，萨瓦亚尔顿金矿床的主要成矿时代为印支晚期， 210ma 。 |
| 4. | 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。 |
| 5. | There are two types of fluid inclusions : petroleum inclusions and aqueous inclusions in the reservoir sandstones . the homogenization temperatures of the aqueous inclusions associated with petroleum inclusions range from 107 to 141
与石油包裹体共生盐水包裹体均一温度107 - 141 ，结合受热史推断出成藏时间在2 . 5my以后。 |
| 6. | The charac teristics of homogenization temperature and salinity data also reports that this high - salinity inclusions were not generated by aqueous fluid immiscibility or boiling in ore - forming processes , but generated directly from a water - saturated crystallizing magmatic melt and that the main mechanism of ore deposition is the mixing of magmatic fluid and underwater not boiling of hydrothermal solution
均一温度和盐度特征还表明，高盐度包裹体不是由热水溶液的不混溶作用或沸腾作用形成的，而是由岩浆熔体直接分离的卤水形成的；沸腾作用对矿质沉淀的作用不大，而流体的混合作用是银山矿床矿质沉淀的主要机制。 |
| 7. | Based on the hydrocarbon accumulation conditions of erlian basin , integrated analyses including burial history , thermal history and characteristics of diagenetic fluid inclusions of oil reservoir in three main depressions are conducted , and in terms of quantitative analysis of homogenization temperature of fluid inclusions , the formation stages of the oil accumulations are determined
摘要在对内蒙古二连盆地3大凹陷成藏条件和埋藏史、热史分析研究基础上，结合储层成岩流体包裹体特征分析，利用流体包裹体均一化温度定量分析方法确定了二连盆地油藏的成藏期，并将二连盆地岩性油藏与构造油藏的成藏期进行了对比研究。 |
| 8. | The analysis results of hydrocarbon generating history , paleotemperature history , the homogenization temperature distribution of fluid inclusions and individual fluid inclusion compounds show that the natural gas charging times in the center gas field is two . the first is at the age of late triassic . at that time , natural gas migrated from the east to the west and from the south to the north
根据鄂尔多斯盆地中部的沉积史、构造发育史、古岩溶形成史、生排烃史等等，按其时空配置关系，归纳气藏的形成可分为四个演化阶段：储集层孕育阶段（ 0 ； c ； ） 、圈闭形成阶段（ c 。 |
| 9. | A large amount of microthermometric data of fluid inclusions indicates that the homogenization temperatures of fluid inclusions in quartz vein from early stage are mainly varied from 270 to 320 , higher than that of main stage which varied from 170 to 250 . 5 . laser - raman analysis for individual inclusions indicate that the inclusions contain co2 , n2 , ch4 respectively
对矿石中的流体包裹体进行了温度、压力、成分、 ph 、含盐度等的分析，并系统地进行了矿床形成时的物理化学条件的理论计算，其中包括eh 、 ph 、 fo _ 2 、 fs _ 2等及金在矿液运移中的搬运形式。 |
