热演化

有机质热演化产生的CO2对孔隙形成具有一定的贡献；

Contribution of CO2 produced by thermal evolution of organic material ;

Ba（1&x）SrxTiO3铁电薄膜的热演化特征与微结构

Pyrolysis-evolution characteristics and microstructures of ba_ ( 1-x ) sr_xtio_3 thin films

随热演化程度的增加，C1含量逐渐减少。相对于正构烷烃的含量，异构烷烃的含量逐渐减少。

With increasing thermal evolution level , the content of methane gradually increases and the content of isoalkanes decreases relative to the content of n-alkanes .

求出各类干酪根在不同的热演化阶段的H/C与R值的回归关系式，并研究了各类干酪根的油气演化界限，讨论了本区的油气勘探前景。

For kerogen at different stages of thermal evolution are given . In addition , the limits of petroliferous evolution of kerogen and explora-tion prospect are discussed .

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 .

对辽河盆地烃源岩的埋藏史、热演化史建立了准三维模型（X、Y和纵向的地质层段，加时间）并编制了相应程序。

The model system , which is an incomplete three-dimensional model ( X , Y , vertical geological layers and time ) about the buried history and the maturity history of source rock in Liaohe Basin , is built and programmed .

本文通过23个点TTI值的计算，建立了TTI与R0的回归方程，划分了6个有机质热演化阶段。

Through estimating the TTI values for 23 points , a regression equation of TTI and Ro is established and 6 thermal evolution stages of organic matters are divided .

按照各地区埋藏历史的特点，可把其划分为Y、N、U、W、V五种类型，各类型的热演化进程不同，有效生气量存在很大差异。

In terms of the characteristics of burial , the basin is classified into regions of 5 different types : Y , N , U , W and V , with varying degrees of thermal evolution and wide discrepancies in the capability of gas generation .

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 .

最后，运用Mckenzie模型模拟了盆地的热演化史。

Finally , Mckenzie ' sstretching model has been used to investigate the thermal history of this basin , Heat flow pattern illustrates that heat flow value at about 6 Ma from now increases abruptly .

应用固体13C核磁波谱分析技术，采用自然演化与热压模拟相结合探讨了干酪根热演化过程中碳骨架与官能团的变化规律，提出脂碳是生烃主要贡献者。

Solid 13C nuclear magnetic resonance spectrometer and natural evolution combining with thermocompression simulator are used for analysis of variation of carbon matrix and functional group in the course of kerogen thermal evolution , showing that lipid carbons mainly contribute to the hydrocarbon generation .

本文用TTI方法研究了烃源岩有机质的热演化史和油气生成史，并结合区内构造发育特征，探讨油气在区域上的运移方向和在时间上的运移期次；

In this paper , thermal evolution history of organic matter of the source rocks and hydrocarbon generation history have been researched by TTI method , hydrocarbon migration direction and migration times were probed combining with the area structure development feature ;

研究表明，在相同热演化程度条件下，除少量样品外，煤层气δ13C1值一般较煤型气偏轻。

The research shows that under the same thermal evolution conditions , the δ 13 C 1 values of CBM is generally lighter than those of coal derived gases , except a few of samples .

Bement和Mango等基于生油岩古地温、热演化史和轻烃分析资料，建立了该轻烃温度参数与埋深温度的函数关系式，用于油气生成温度计算。

Based on the paleogeotemperature , the thermal history and the analytical data of light hydrocarbon for source rocks , Bement and Mango et al . established the functional equation between the light hydrocarbon temperature parameter and the burial temperature and applied it to the calculation of hydrocarbon-generating temperature .

超压环境有机质热演化和生烃作用机理

Kinetics of organic matter maturation and hydrocarbon generation in overpressure environment

聚苯醚/聚苯乙烯共混物溶液浇铸膜的热演化行为

Thermal Evolution Behavior of Solution-cast Film of PPO / PS Blends

中牟凹陷热演化特征及其资源评价

The Zhongmou depression evolutionary feature in hydrothermal stage and resource assessment

为腐泥型有机质，热演化已经处于过成熟阶段。

They are sapropelic and over - mature in thermal evolution .

苏北盆地高邮凹陷热演化史研究

Study on Geothermal Evolution History of Gaoyou Sag in Subei Basin

南华北地区石炭系-二叠系有机质热演化成因类型研究

Carboniferous-Permian Organic Mass Thermal Evolution and Genesis in South Huabei Area

渤海盆地热历史及构造-热演化特征

Thermal history and tectonic-thermal evolution of Bohai basin , East China

岩浆成矿体系的热演化和剥露史的数字模拟

Numerical Modelling of Thermal and Exhumation Histories of Magmatic Ore Deposits

应用磷灰石裂变径迹定量恢复热演化史

Quantitative method of recovering thermal evolution history with apatite fission track

盘星藻烷烃生物标志物特征及其热演化试验的初步研究

A preliminary study on hydrocarbon biomarkers and thermal alteration of Pediastrum

云龙凹陷构造-热演化史分析

Tectonic - thermal evolution analysis of Yunlong Sag , Chuxiong Basin

岩石圈流变性对拉张盆地构造热演化历史的影响

Effects of lithospheric rheology on Thermal-mechanical modeling of extensional basins

利用磷灰石裂变径迹资料反演热演化史的综合分析法

The combinative analysis method of thermal history inversion with apatite fission tracks

济阳坳陷惠民凹陷热演化史分析

An analysis of thermal evolution history of Huimin Sag in Jiyang Depression

甲基菲比值与有机质热演化的关系

The Relationship between Methyl Phenanthrene Ratios and the Evolution of Organic Matter

海相不同类型烃源岩有机质丰度热演化规律

Thermal evolution pattern of organic matter abundance in various marine source rocks