1) Indoor Temperature Swing
室温均一化
2) homogenization temperature
均一化温度
1.
The analysis result of the homogenization temperature of the fluid inclusions shows that there are two petroleum injections.
柴达木盆地西部第三系盐湖相烃源岩成熟期为晚第三纪,成烃期相对较晚;盆地西部大部分构造圈闭是在晚第三纪末—第四纪形成,只有少数构造圈闭是在早第三纪末期形成,总体上讲构造圈闭形成比较晚;流体包裹体均一化温度测定结果表明,盆地西部油气藏存在两次充注,第一次是在晚第三纪早期,第二次是在晚第三纪末期,充注期次相对比较晚;对成藏期次综合分析后确定盆地西部油气成藏时期比较晚,为柴达木盆地油气藏形成的一大特点。
2.
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。
3) homogeniation temperature
均一化温度
1.
GOI(grain with oil inclusion) value, the homogeniation temperature and MCI(molecular composition of inclusion) can be used to determine the paleo-OWC(oil water contacts), the charging time and hydrocarbon charge history respectively.
含油包裹体丰度(GOI)可以确定古油水界面,包裹体均一化温度可以确定油气藏形成时间,包裹体分子组成可以反演油藏的充注历史,冰点可以确定地层水的演化及确定油藏储量。
2.
GOI( grain with oil inclusion) value, the homogeniation temperature and MCI(molecular composition of inclusion) can be used to determine the paleo-OWC(oil water contacts).
含油包裹体丰度GOI可以确定古油水界面,包裹体均一化温度可以确定油气藏形成时间,包裹体分子组成可以反演油藏的充注历史,冰点可以确定地层水的演化及确定油藏储量。
4) homogenization temperature
均一温度
1.
A discussion on hydrocarbon accumulation dating determined by homogenization temperature and burial history of fluid inclusions——An example from the Fushan depression,Beibuwan basin;
由流体包裹体均一温度和埋藏史确定油气成藏时间的几个问题——以北部湾盆地福山凹陷为例
2.
The time of petroleum accumulation in the Shiwu fault depression of the southern Songliao basin is determined according to the studies of structural evolution,hydrocarbon-generating history of source rocks and homogenization temperature of fluid inclusions.
通过对松辽盆地南部十屋断陷构造发育史、烃源岩的生烃史、流体包裹体均一温度的研究,综合分析了盆地的成藏期次。
3.
Microscopic inspection,microthermometry and salinity measurement,systematic fluid inclusion studies in the Qingshen gas field of the Songliao Basin show that homogenization temperature of fluid inclusion varies from 97.
松辽盆地北部庆深气田储层火山岩的流体包裹体均一温度为97。
5) uniform temperature
均一温度
1.
根据储层的成岩序次、油气包裹体特征及含烃盐水包裹体均一温度,结合构造活动特征及烃源岩演化史,对歧口凹陷马东东地区沙一段下亚段油气藏进行了成藏期次综合研究。
2.
By using the testing results of its composition, fluorescence, uniform temperature, isotope and so on, the conditions of tectonic fluid inclusion in oilgas migration and preservation are studied; the application to mechanical property, stress field of the faulting is presented.
利用构造流体包裹体的成分、荧光、均一温度及同位素等测试结果,分析研究了其在油气运移和保存条件,以及断裂的力学性质、应力场等方面的应用,并探讨了存在的问题及发展方
3.
Contained gas horizon inclusion in Upper Palaeozoic Erathem of Shenmu area is investigated by measurement of its uniform temperature and freezing point and application of fluorescence analysis and laser Raman composition analysis.
通过包裹体均一温度和冰点的测定以及应用荧光分析、激光拉曼成分分析等方法对榆林—神木地区上古生界含气层位包裹体进行分析表明,该区主要存在盐水包裹体和烃类包裹体。
6) homogeneous temperature
均一温度
1.
Based on the analysis of homogeneous temperature,salinity,biomarker,color spectrum and color-mass spectrum in fluid inclusion,the geochemical feature of primary(paleo) hydrocarbon component of reservoirs was restored,their geochemical evolution was uncovered,and oil sources and hydrocarbon thermal evolution were both tracked in this paper.
根据对流体包裹体均一温度、盐度、有机包裹体中的生物标志物特征研究及有机包裹体的色谱、色—质谱分析,恢复储集岩中初始(古)油气组分的地球化学特征,揭示储集岩中油气组分地球化学演化过程,追踪油气藏的油源及油气的热演化程度,最后分析柴北缘油气的充注期次认为,冷湖构造带和南八仙油气田在成岩演化及油气的充注、运移方面存在一定差异,其中冷湖构造带内冷七1井N12地层只有一期油气充注,潜参1井、冷四1井和深86井均有E3和N1—N12两期油气充注,而南八仙油气田仙5、仙6、仙7井样品中两期充注的油气分别形成于E3—N1和N2时期。
2.
The type distribution,homogeneous temperature and components of organic inclusions in authigenic quartz of sandstone,member 3,Lingshui formation show that gas migration began at Pliocene,in Ya 131 gas field.
通过对琼东南盆地崖１３－１气田陵水组三段储层砂岩自生石英中有机包裹体的类型分布、均一温度及成分等的研究认为，崖１３－１气田天然气开始运移的时间在上新世，运移深度为３。
3.
Based on the comparison of the composition and homogeneous temperature of salt-water inclusions with hydrocarbon between Well Aran2 and Well FKH1 in Iran Qom Basin,this paper reveals the process of oil/gas injection and accumulation.
通过对伊朗库姆盆地Aran2井和FKH1井含烃盐水包裹体成分和均一温度的对比研究,揭示油气充注和成藏过程。
补充资料：敏化室温磷光法
分子式：
CAS号：
性质： 一种基于能量转移的流体室温磷光法。本征无磷光或磷光很弱的物质（供体）被激发到三线态后，将其能量转移给某种物质（受体），并产生一个具有高磷光量子产率的受体三线态，利用受体三线态的室温磷光（RTP）发射特性可实现供体的测定。实现S-RTP应满足：受体三线态能量低于供体三线态能量，且有高的磷光量子产率；在供体的激发波长处受体无吸收，或吸收可忽略。常用的受体有联乙酰和1，4-二溴代萘。
CAS号：
性质： 一种基于能量转移的流体室温磷光法。本征无磷光或磷光很弱的物质（供体）被激发到三线态后，将其能量转移给某种物质（受体），并产生一个具有高磷光量子产率的受体三线态，利用受体三线态的室温磷光（RTP）发射特性可实现供体的测定。实现S-RTP应满足：受体三线态能量低于供体三线态能量，且有高的磷光量子产率；在供体的激发波长处受体无吸收，或吸收可忽略。常用的受体有联乙酰和1，4-二溴代萘。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条