Simulating Experiments Combined with GC-IRMS: Application to Effective Source Rock Research
Study of Carbonate Source Rocks Evaluation Criterion
Geology, Geochemical Characteristics and Mechanism of Hydrocarbon-generating for Source Rocks from the Tertiary Salty Lacustrine Facies in the West Region of the Qaidam Basin
Research and Application of Assessment Methods to Source Rock in Binbei Area of Songliao Basin
Geo-macromolecular Structure of Organic Matter in Immature Source Rocks and the Mechanism of Immature Petroleum Formation
BIOLOGICAL ORIGIN OF EARLY PALAEOZOIC AND PRECAMBRIAN HYDROCARBON SOURCE ROCKS BASED ON C_(27)/C_(29) STERANE RATIO AND ORGANIC CARBON ISOTOPE
The organic matters of Types Ⅰ,Ⅱ 1,Ⅱ 2,and Ⅲ were found out in the hydrocarbon source rocks in Dongying Formation , in which the Types Ⅱ 1 and Ⅱ 2 are in the majority.
东营组 烃源岩Ⅰ、Ⅱ1、Ⅱ2 和Ⅲ型有机质均有分布,但以Ⅱ1、Ⅱ2 型为主;
Major hydrocarbon source rocks are in the Cambrian and Ordovician.
寒武-奥陶系 烃源岩是该区主力 烃源岩;
The geochemistry character of the Well Fu 1 and Bal 1 suggests that the horizon developed in the middle interval of the Abu Gabra Formation is the low matured good to excellent source rock. It is supposed that the hydrocarbon source rock in the deeper could be higher mature.
分析Fu 1井与Bal 1井 烃源岩地球化学特征 ,下白垩统AbuGabra组中段 烃源岩为低熟—成熟的好—极好 烃源岩 ,推测埋藏较深部位的 烃源岩成熟度较高 ,资源潜力较大 ,认为福拉凹陷是M盆地最好的生油凹陷。
The thicknesses of the effective Jurassic muddy hydrocarbon source rock and carbonate hydrocarbon source rock are generally 100 to 500 meters and 200 to 600 meters,respectively. There are hydrocarbon-rich rocks with 200 to 400 meters thick devceloping in J_2x and J_3s formations.
侏罗系有效泥质 烃源岩厚度一般在100~500 m,有效碳酸盐 烃源岩厚度一般在200~600 m,J2x和J3s局部地区发育有200~400 m的富 烃源岩;
The result shows that hydrocarbon retention amount in source rock is 5. 438 × 1010t (oil equivalent), accounting for 67. 9 % of the amount of hydrocarbon generated;
计算出吐哈盆地前侏罗系的 烃源岩残留烃量为 5． 438 × 1010t（油气当量），占生烃量的 67． 9％；
The study of organic matter in source rock by using supercritical CO_2 extraction
The averagecontent of naphthalene series is 22. 16% in crude oils, but is 22. 25% in source rocks.
From the yield and composition changing characteristic of gas, water is one of the most important factors to hydrocarbon generation in source rock at the range of experimental temperature.
从气态的产量及组分变化特征上来看,在研究温度范围内,水是 烃源岩中有机质成烃演化的重要因素之一,水不仅是 烃源岩中有机质成烃演化的重要氢源,而且水的酸碱性也是 烃源岩中有机质成烃演化的重要因素之一;
Experimental study on absorbability of methane in source rocks
Continual hydrocarbon sources or conditions of various late-period accumulations are the preconditions for Paleozoic oil-gas accumulations being conserved during the geological history.
因此,古生代形成的油气藏(田)要在地史过程中保存下来,必须不断有 烃源补给,或是具备各种晚期成藏的条件,诸如 烃源岩晚成熟、构造圈闭晚定型以及次生油气藏的形成等等。
The high abundance in organic matter, good in type, great thickness in sedimentation, and strong in hydrocarbon generation, all these can supply sufficient hydrocarbon sources for forming oil and gas pool of medium type to large type.
有机质丰度高 ,类型好 ,沉积厚度大 ,生烃强度大 ,能为形成大中型油气藏提供充足的 烃源。
In West Sichuan Depression,the hydrocarbon sources of T 3 are abundant and the sandstones in it are developed.
Multitudes of hydrocarbon sources and kitchens have provided abundant hydrocarbon sources for the formation of lithologic reservoirs.
Study on hydrocarbon sources of Lower Triassic Jialingjiang Formation in south of Sichuan Basin, China
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9-O-methylfusarubin was isolated from a novel source, Fusarion oxysporum, and evaluated for its phytotoxic and chlorotic inducing properties in plants as well as its potential as an antineoplastic agent.
This note shows that for a BVP of Poisson's equation withQm(u, v) as its source function, a direct evaluation of some integrals yields the same exact results as obtained by similarity analysis.
The nonlinear PDEs consist of a heat equation with the Joule heating as a source and a current conservation equation with temperature-dependent electrical conductivity.
In order to get these second-order error estimates, the Joule heating source is used in a changed equivalent form.
A nonlinear degenerate parabolic equation with non-local source
Some faults connected the deep-water fans with the hydrocarbon source.
In the end, according to the structural evolution and hydrocarbon source rock depositional distribution, the distribution of deep-seated gas in China is predicted.
On the geobiological evaluation of hydrocarbon source rocks
Hydrocarbon source rocks are characterized by the hydrocarbon discharge, and the alteration and variation in organic compositions and organic content due to the enhanced thermal maturation.
Understanding the dynamics of organic matter in modern marine water columns greatly favors the geobiological evaluation of hydrocarbon source rocks.
These variations throw constraints on the application of the conventional inversion evaluation of hydrocarbon potential by assessing the residual organic matter left in source rocks.
The alloplasmic hybrid was more tolerant to decreased source strength in source-sink relations as compared to the initial cultivar.
An increase in source concentration towards the center of the layer intensifies the effect.
Procedures for the determination of impurity components in source materials by gas chromatography with flame-ionization detection were developed.
The possible contents of OM (Corg) and U were reconstructed in source rocks of metasediments of the Lapland-Kolvitsa granulite belt of the Baltic Shield.
Primary heavy oil is generated directly by Cretaceous immature or low-mature hydrocarbon sources, or is derived from differentiation of crude oil during migration.
The use of several molecular markers and related indexes derived for n-alkane and PAHs has been proposed for assessing the relative contributions to the environment of hydrocarbon sources.
The 20th century saw the prolific exploitation of fossil hydrocarbon sources (coal and oil) which are finite and exhaustible.
The presence of hydrates in the upper 1000 m of sediments also can be considered as an indicator of deeper hydrocarbon sources.
The activation energy in the range of 46.9-51.1 kcal/ mol is obtained in the initial stage of 3C-SiC growth for both hydrocarbon sources.