生油

该系列油类灌装线广泛适用于灌装各种油类及粘稠液体，如花生油、调和油、菜籽油等食用油的灌装。

Main Purpose : . This series of oil filling line widely used in various oil and filling viscous liquid , such as peanut oil , blend oil , canola oil filling .

某井生油岩中C1&C7轻烃组成的地球化学意义

Geochemical significance of light hydrocarbon composition in source rocks of a test well

应用显微FTIR光谱技术原位研究沉积岩中生油母质干酪根

Situ-Study on Generative Kerogen in Sedimentary Rock by FTIR-Microspectrometry Technique

X射线荧光光谱成型滤纸片法测定生油岩抽提物中的钒和镍

Determination of vanadium and nickel in the extract of source rocks by X-ray fluorescence spectrometry with formed filter paper method

Wood（1988）所提出的TTI值和计算方法及R0值的关系，确定研究区生油、气门限，并分析了有机质成熟度的热演化史。

Wood 's method ( 1988 ), the writers confirm the oil and gas and analyse the maturity of organic material hot evolution histories .

用TTT法定量评价生油岩

Quantitative evaluation of source rocks with TTT method

成熟度参数表明原油成熟度相当于Ro值为0.8%~1.0%阶段，是生油高峰阶段。

The oil mature parameter indicates that the oil is at the generation peak and equal to a stage of R_o from 0.8 % to 1.0 % .

本文应用轻烃（C1-C7）分析结果，研究了一个碳酸盐岩含油气盆地泥盆系至三叠系的原油和生油岩的轻烃特征。

Characteristics have been studied of volatile hydrocarbon ( C1-C7 ) from oils and oil source rocks of Devonian to Triassic ages in Jurong carbonate basin .

计算生油气量的C-K法

The c-k calculation method of oil formation

TTI计算表明其主要烃源岩主要生油期为晚白垩世。

The value of TTI shows that hydrocarbon is largely generated at late Cretaceous for the primary source rocks in Chagan sag .

显微荧光分析表明，镜质组反射率Ro在约0.7%左右时，次生荧光大量出现，并随成熟度增加而逐渐增加，标志着大量生油的开始。

Micro fluorescence analysis of the coals shows that large amount of secondary fluorescence occurs when vitrinite reflectance is about 0.7 % , moreover , its intensity increases with the increase of maturity .

在校正时选1%作为生油高峰对应的镜质体反射率（RO），在不同盆地或对于不同类型烃源岩可能有所不同，应根据某一盆地的烃源岩实测演化剖面来选定生油高峰对应的RO。

The selection of vitrinite reflectance at oil-generating peak when correction should be based on measured source rock evolutive section in a basin for different basins or different source rocks have somewhat different vitrinite reflectance .

三叠系烃源岩Ro值的分布范围为0.60%~2.59%，均值为1.1%，主体处于生油晚期。

While that of Triassic source rock is in its late period of oil generation , with R_o value in the range of 0.60 % - 2.59 % and average value of 1 . 1 % .

应用该模型测算了江汉盆地JJ、QQ、XX凹陷潜江组未熟烃源岩在现今的累积生油强度和生油量。

By using this model , the current cumulative oil generating intensity and amount for immature source rocks of Qianjiang formation were calculated in JJ , QQ , XX Depressions , the Jianghan Basin .

进而可以研究油气藏的油源&生油岩的类型和热演化程度。本文评述了依据油相包裹体和同生水溶液包裹体PVT相图推断其捕获温度和压力范围的有效性和局限性。

Furthermore , the efficiency and limitation of the method to determine the entrapment temperatures and pressures of fluid inclusions based on PVT diagrams of oil inclusions and associated aqueous inclusions are evaluated .

库车前陆盆地侏罗系烃源岩Ro值为0.55%~1.88%，均值为0.93%，主体处于生油高峰期；

The main body of Jurassic source rock in Kuqa foreland basin is in its peak of oil generation , with R_o value in the range of 0.55 % - 1.88 % and average value of 0.93 % .

作者针对生油热解分析中，进样量和升温速率的改变，引起S2、Tmax相应的变化等问题，做了系统的试验，并提出了进样量的合理值。

In view of the problems of the variation of S2 Tmax values due to the changes of the amount of injection and heating rate , systematic experiments have been done .

生油岩荧光光谱特征为：荧光强度大（＞40）λmax在450nm左右，光谱位于蓝绿光区，演化程度属高成熟原油阶段。

Fluorescence spectral characteristics of the oil-generating rocks are : strong fluores-cence intensity ( > 40 ), around 450 nm , and spectra being located in the blue-green light region , indicating a high-maturity oil stage .

热水流体在地球内普遍存在，且常常进行大规模的迁移，在地表以下2km往往就可形成达到生油要求的门限温度。

The hydrothermal fluids which can be formed below the surface of the earth about 2 km are ubiquitous in the crust and it migrate generally in large scale .

生油窗为31006300m，成油期为40180Ma。

The oil generation window occurs between 3100 and 6300m , and the oil generation period was from 40 to 80 Ma .

如埋深为2768m时，生烃率为0.05（可视为生油上限）；

For example , at a depth of 2768m , the rate of hydrocarbon formation is 0.05 ( upper threshold );

在实验室条件下，利用压力差热分析仪（DTA）分别对新疆和吉林两种生油岩做了压力热解实验。

For a better simulation of the natural degradation of source rock Kero - gen under experimental conditions , pyrolysis experiments on two kinds of source rock samples from Xinjiang and Jilin were carried out by means of high pressure differential thermal analyser ( DTA ) .

模拟结果表明：辽河盆地生油量为700.8×108t，生气量为59.6×1011m3；

The simulation result shows : the oil generating amount in Liaohe Basin is 700.8 × 10 8 t , and its gas generating amount is 59.6 × 10 11 m 3 ;

Qom组在新生代中晚期（约4Ma-5Ma）盆地快速沉降阶段进入生油阶段，而此时侏罗系已达到过成熟阶段，大量生成干气。

Source rocks in Qom formation entered hydrocarbon generation stage for the basin quickly subsidence in late Cenozoic ( about 4-5Ma ), meanwhile source rocks in Jurassic have entered highly matured stage , generated lots of gas .

西湖凹陷主要生油岩是下第三系暗色泥页岩，其大量生成油气的温度约为90℃，生油门限是2800m左右。

Dark shales are believed as major oil source rocks in Xihu depression , which got to the oil generating threshold at about 2 ? 800 m corresponding to 90 ℃ .

结果表明，绝大多数生油岩有机碳含量大于0.90%，氯仿沥青A含量平均值大于600ppm，总烃大于200ppm。母质类型为腐殖腐泥型和腐泥腐殖型。

The organic matter abundances show that content of organic carbon is more than 0.9 % in most source rocks and that of Chloroform asphalt " A " is generally greater than 600 ppm and hydrocarbon greater than 200 ppm .

结果表明，该凹陷中心Es3生油岩主生油期出现在20～14Ma，主生气期出现在15～10Ma；

The results have shown that the Es 3 source rock from the depression center was matured to the main stage of oil generation and the main stage of gas generation occurred over stage of 20 ~ 14 Ma and 15 ~ 10 Ma , respectively .

应用Easy-Ro（%）数值模拟方法对下白垩统烃源岩生烃史的研究表明，本区主要生油期为晚第三纪-第四纪，不存在二次生烃作用。

Applying the Easy-Ro ( % ) model to the hydrocarbon generating history research of the lower Cretaceous source rocks shows that the main oil-generating period is from late Tertiary to Quaternary , and does not exist the second hydrocarbon-generating event during the geological time .

白垩系在全区的残留面积为39675km2，最大残留厚度为5200m，有利于有机质的生成和转化，预示了白垩系较好的生油能力。

The remained Cretaceous deposit in the whole region is 39 675 km ~ 2 in area , with a maximum thickness of 5 200 m , hence presenting good conditions for the generation and transformation of organic matter and indicating a better oil and gas potential in this region .

乐平煤系树皮煤生油研究陕北石油秩序

Research on bark coal - formed oil in Leping coal measures