填充树脂岩的生烃特性将取决于填充树脂的性质。
The hydrocarbon-generating characteristics of filled resinite would depend on the properties of filled resins.
藻类体是该区低熟油的重要生烃组分。
Alginite is the main hydrocarbon generating macerals for the low mature oil.
因此，在地球深处应存在合成生烃机制。
Therefore, there should be the case of synthetic hydrocarbon generation mechanism in deep of the earth.
油气主要分布在富生烃凹陷西侧的隆起上。
Those sags along the detachment faults are prolific oil gas depressions.
煤的生烃性与主要生烃组分的含量密切相关。
The hydrocarbon generation characteristics of coal correlates closely with the quantities of hydrocarbon generation maceral.
腐植型干酪根的加氢生烃效应在各个阶段都较显著。
While for humic kerogen, hydrocarbon production by hydrogenation can be increased at every stage of thermal evolution.
壳质组和腐泥组含量与组成决定了烃源岩生烃特点和潜力。
The content and composition of exinite and sapropelinite determine the hydrocarbon-generating feature and potential of source rocks.
对二次生烃机理进行了讨论，认为二次生烃与一次生烃连续。
Mechanism of secondary hydrocarbon generation was discussed and considered to be continuous with the primary generation.
矿物结合有机质可作为碳酸盐岩生油岩的一种重要生烃物质。
The organic matter, enclosed in carbonate minerals, is an important hydrocarbon producing substance in carbonate source rocks.
在中低温度下单质硫可以大幅度提高生烃母质可溶物质产率。
Sulphur can greatly promote the productivity of soluble matters from hydrocarbon source rock under the condition of middle-low temperature.
化学反应动力学是评价煤的生烃过程和生烃特性行之有效的方法。
Chemical reaction kinetics has been considered as an effective method for assessing the process and characteristics of hydrocarbons generation from coal.
这些烃源岩均具有有机质丰度高、生烃潜力大和非均质性强的特点。
The hydrocarbon source rocks all have high abundance of organic matter, high hydrocarbon potential and show great heterogeneity.
据富氢程度将煤与分散有机质进行对比，则煤具有更大的生烃能力。
Niqiuji depression, coal-bearing system, dispersed organic matter and coal, hydrocarbon potential, Carboniferous-Permian.
下扬子盆地属改造型海相盆地之一，具有多期生烃、多次成藏的特点。
The Lower Yangtze basin is a modified marine basin, characterized with multi-stage hydrocarbon generation and reservoir formation.
矿物低温催化脂肪酸或酯的脱羧生烃是石油成因机制的一个重要方面。
It is an important aspect in cause of petroleum formation that hydrocarbon from fatty acid or ester decarboxylation catalyzed by minerals at low temperature.
压实不均衡和生烃作用分别是本区超压发育、演化不同阶段的主控因素。
Compaction disequilibrium or hydrocarbon generation is main controlling factor of different phases for the development and evolution of overpressure.
油气从高压应力分布区(生烃凹陷)向低压应力分布区(隆起区)运移。
The migration of hydrocarbon tends to take place from high pressure stress distribution area (hydrocarbon generation sag) towards low pressure stress distribution area (uplift).
通过热模拟实验的方法，探讨了复杂生烃史条件下烃源岩生烃量的变化特征。
The hydrocarbon-generation amounts under the complex geological history in poly-cyclic basin were discussed through several sets of thermal simulation experiments.
本文描述塔里木盆地晚奥陶世塔中北斜坡带良里塔格组的生烃生物组合特征。
This paper deals with the feature of bio-precursors of hydrocarbon in Lianglitake Formation, Late Ordovician of north-slope of Central Uplift of Tarim Basin.
作者通过逐阶抽提加热和逐阶加热模拟实验对碳酸盐岩的生烃机理进行了研究。
The mechanism of hydrocarbon generation in carbonate rocks are studied by step heating extraction and simulation.
持续生烃和压实封闭是普遍超压的主因，现代地压状况是晚期构造改造的结果。
The superpressures mainly result from sustained hydrocarbon-generation and compaction seal and the current geopressure circumstances are the result caused by late tectonic movements.
烃源岩的构造-受热史是有机质成熟演化、烃源岩生烃演化的最重要控制因素。
It is the most important that source rocks tectonic heated history to maturity of organic matter and controls on the hydrocarbon generation of source rocks.
下三叠统海相烃源岩是下扬子区最有利的烃源岩，陆相沉积也具有一定的生烃潜力。
The Lower Triassic Marine source rock is the most favorable one in the Lower Yangtze area, and the continental deposit has certain hydrocarbon generating potential.
在经历后期构造改造后，盆地的晚期生烃及晚期油气运移受改造后的构造格局控制。
After the late structural transformation, the late sourcing period and the late oil and gas migration in the basin are controlled by post-transformation structural configuration.
含油气系统中的生烃时间、排烃时间及聚集时间由生物标志化合物的分析与对比确定。
The time of hydrocarbon generation, expulsion and accumulation could be determined through the analysis and correlation of biomarkers of the system.
潜江凹陷蚌湖向斜是下第三系潜江组的沉积中心，是江汉盆地油气最富集的生烃中心。
Banghu syncline in the Qianjiang sag is a depocenter of Paleogene Qianjiang Formation, and is the richest hydrocarbon generation center in Jianghan Basin.
受沉积剥蚀及盆地构造—热演化的控制，生油岩系的生烃阶段与过程具有多期次的特征。
Controlled by the deposition and erosion as well as the basin thermal evolution, the hydrocarbon generation was of multi-phases.
有机生烃除常规的区带生烃模式外，应对灶体生烃模式及催化生烃模式引起足够的重视。
Excepting zonal hydrocarbon generation model, kitchen and catalytic models of organic hydrocarbon generation mechanism should be taken into considerable account.
通过对沉积埋藏史、生烃史及油气运聚史的研究，确定烃源岩生、排烃及油气运聚期次；
The stages of oil generation, expulsion, migration and accumulation are determined through study of depositional history, oil generation and migration and accumulation history.
通过对沉积埋藏史、生烃史及油气运聚史的研究，确定烃源岩生、排烃及油气运聚期次；
The stages of oil generation, expulsion, migration and accumulation are determined through study of depositional history, oil generation and migration and accumulation history.
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