Typical organic constituents of kerogen are algae and woody plant material.
干酪根的典型有机组分为藻类和木质植物。
The other is normal mature crude oil from the thermal degradation of kerogen.
另一种是正常的干酪根热降解成熟原油。
Natural gas is not only originated from kerogen cracking, but also from oil cracking.
天然气既可来源于干酪根的裂解气，也可来源于原油的裂解气。
Sapropelic gas could be derived from the cracking of both sapropelic kerogen and sapropelic crude oil.
腐泥型天然气既可来自腐泥型于酪根的裂解，也可以来自腐泥型原油的裂解。
Generation of hydrocarbon from kerogen is one of important genetic types of abnormal pressure in source rock.
干酪根热解成烃作用是烃源岩中异常高压的重要成因之一。
Tectonic activities and volcanism in the basin have an influence on hydrocarbon generation of kerogen and its change.
盆地构造活动和火山作用可以促进干酪根的成烃转化。
While for humic kerogen, hydrocarbon production by hydrogenation can be increased at every stage of thermal evolution.
腐植型干酪根的加氢生烃效应在各个阶段都较显著。
A new type of kerogen automatic preparation instrument can automatically operate the whole process of kerogen preparation.
一种新型干酪根自动制备仪能自动完成干酪根制备工作的全过程。
Whole rock analysis and kerogen analysis are two analytical methods of studying hydrocarbon source rock in organic petrology.
全岩分析与干酪根分析是有机岩石学研究烃源岩的两种分析方法。
The element composition and mature of kerogen is an important distinguish mark between great and small scale carlintype gold deposits.
干酪根的元素组成和成熟度是判别大型卡林型金矿床和小型卡林型金矿床或矿点的重要标志。
The analytic results of kerogen-like material samples show that bacterially degraded algal cells have a tendency to gelation during pyrolysis;
类干酪根分析结果表明，细菌降解的藻细胞在热解时更易凝胶化；
The free radicals in kerogen of sedimentary organic matter can be easily determined by using the electron paramagnetic resonance(EPR) technique.
利用电子顺磁共振（EPR）技术可以简便地测定沉积有机质中干酪根的自由基。
The free radical concentration (Ng) of kerogen is a valid index to study thermal maturation of organic matter and paleotemperature of sedimentary basin.
干酪根自由基浓度是研究有机质热演化的有效指标之一。也是研究沉积盆地古地温的热参数之一。
With supercritical hydroextraction, in which an H-donor is added to the supercritical toluene, a complete recovery of kerogen with high oil yield is possible.
在溶剂甲苯中加入少量供氢组分后，油母转化完全，油类产物产率高。
Microscopic studies of the kerogen from the chert samples show that the main components of the kerogen are organic fragments and microsome with weak anisotropy.
油浸显微镜下鉴定硅岩中的干酪根组成多为有机质碎片和微粒体，并显示微弱的各向异性。
The wide existence of immature oils throughout the world especially in China broke through the hydrocarbon generation theory through kerogen thermal degradation.
世界上特别是中国未成熟石油的普遍存在，突破了干酪根热降解成烃的理论模式。
Considering complex preparation of kerogen in the petrochemical field, This paper introduces a program of kerogen complex preparation control system based on CAN bus.
本文针对石油化工领域中干酪根复杂制备过程，提出了一种以CAN总线为基础的干酪根自动制备控制系统方案设计。
By using simulation experiments, TGA method and Rock-Eval analysis, the potential of kerogen for oil generation was measured and compared with that determined by Tissot.
本文还用实验模拟、热重、热谱等方法测定了干酪根的生油潜量，并与蒂索确定的生油潜量进行了比较研究。
A sequential selective chemical degradation was performed for the kerogen from the Nenjiang Formation of the southern Songliao Basin by using a series of mild chemical degradations.
采用一系列温和的化学降解法对松辽盆地南部嫩江组烃源岩的干酪根进行连续的选择性化学降解，并对不同降解产物进行色谱—同位素比值质谱分析。
This paper discusses systemically the application of whole rock analysis in the study of terrestrial source and compared with the results obtained from conventional kerogen analysis.
本文从有机岩石学的角度，系统论述全岩分析在陆相烃源岩研究中的应用，并与传统的干酪根分析进行对比。
The microcrystalline parameter bears a direct relationship to the evolutionary level of the kerogen, i. e. the higher the maturity, the higher the value of the microcrystalline parameter.
微晶参数与干酪根的演化程度有关，成熟度越高微晶参数值也越高。
Dongying North part deep sand Shasi low Subsegmental of gas condensate methane and ethane are lighter isotopes shows that Cracking gas oil characteristics, rather than kerogen pyrolysis gas.
东营北带深层沙四下凝析油气甲乙烷同位素均较轻，表现出明显的原油裂解气特征，而非干酪根裂解气。
Thermal simulation experiments of kerogen samples show that free radical concentration would first increase and then decrease along with increasing thermal evolution degree of kerogen samples.
干酪根样品热模拟实验结果表明，随着干酪根热演化程度的增高，自由基浓度表现出先升后降的变化特征。
Kerogen type is mainly humic, and terrestrial higher plants are the petrologen.
干酪根类型以腐殖型为主，成烃母质为陆地高等植物；
Kerogen is the leftover material of sporopollen element and lignin in original bodies in different thermal metamorphic period and it is the original material of gas-oil formation.
干酪根主要是母源体中的孢粉素与木质素在埋藏环境中不同热变质阶段的残留物，是油气形成的母源物。
The coal-formed oil is characterized by heavy end components, high wax content and high viscosity which is determined by Kerogen, maturity and expulsion mechanism in the coal-bearing Jurassic.
侏罗系煤中特定的生油母质、有机质成熟度及排驱机理决定了煤成油的重质、高蜡和高粘度特点。
The coal-formed oil is characterized by heavy end components, high wax content and high viscosity which is determined by Kerogen, maturity and expulsion mechanism in the coal-bearing Jurassic.
侏罗系煤中特定的生油母质、有机质成熟度及排驱机理决定了煤成油的重质、高蜡和高粘度特点。
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