kerogen
n. [地质][油气] 油母巖质
2026-04-13 14:20 浏览次数 27
n. [地质][油气] 油母巖质
1. bituminous material occurring in shale and yielding oil when heated
kerogen oil也称干酪根石油
kerogen sapropelite干酪根腐泥巖
liptinite kerogen类脂质型干酪根
kerogen cracking干酪根的裂解
petrologen[地质][油气] 油母巖质;油母质
algae kerogen藻干酪根
humic kerogen腐殖型干酪根
kerogen rock干酪根巖
coaly kerogen煤质油母质
kerogen concentrate干酪根富集体
in this paper, we have polled the method determining the aromatic degree of kerogen by x-ray diffraction.
本文探讨了用x光衍射技术,测干酪根芳香度的方法。
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。
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 cracking gas from oil is very different from the cracking gas from kerogen in components and carbon isotopes.
原油二次裂解生成的天然气与干酪根初次裂解生成的天然气在组分特征和碳同位素特征上存在明显的差异。
meanwhile, tow different calibration methods of fixed preexponential factors and alterable preexponential factors of kerogen with different structure.
提出了对不同复杂结构的干酪根样品固定指前因子法和变指前因子法的两种标定方法。
this paper presents the thermal modelling of hydrocarbon generation from different types of kerogen and coal by a combination technique of programmed heating microscope stage and video recording.
本实验利用显微热台装置,配合程序升温,对不同类型的干酪根和煤进行热模拟实验,并运用显微录像进行连续观察和记录。
the kinetic models commonly used are proposed that the reactions of hydrocarbon generation from kerogen are parallel and independent.
目前,常用的模型都是基于干酪根裂解生烃由一系列相互独立平行一级反应组成的假设基础上。
the in situ visualization of pyrolysis of kerogen and asphalt in high-temperature and high-pressure water studied by hydrothermal anvil cell.
采用热液对顶砧压腔装置,对高温高压水中干酪根和沥青质的热解过程进行了原位观测。
carbon isotopic value of methane from similitude kerogen is lighter than that from total rock in the presence of element sulfur.
单质硫的存在会导致普遍出现假干酪根甲烷碳同位素值轻于全巖甲烷碳同位素值;
whole rock analysis and kerogen analysis are two analytical methods of studying hydrocarbon source rock in organic petrology.
全巖分析与干酪根分析是有机巖石学研究烃源巖的两种分析方法。
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。
black shale is the most favorable lithofacies which has high organic abundance and greatest kerogen type(mainly type i). laminar mudstone is the second favorable lithofacies.
黑色页巖巖相有机质丰度高,有机质类型以i型干酪根为主,是最有利的富有机质巖相类型,其次为纹层状泥巖巖相。
the formation of hydrocarbons from a source rock as bitumen forms from kerogen and accumulates as oil or gas.
烃类从源巖中形成的作用,如由干酪根形成沥青并聚集成油或气。 亦称生成作用。
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。
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。
a simulation experiment was made on kerogen from shales in the lower xiamalin formation of the proterozoic in north china.
本模拟实验主要对华北上元古界下马岭组页巖干酪根的热演化特征和规律进行研究。
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。
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。
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。
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巖中异常高压的重要成因之一。