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最后是一种叫做油母质的大分子化合物。and macromolecular clumps of organic material called kerogen.

干酪根的典型有机组分为藻类和木质植物。Typical organic constituents of kerogen are algae and woody plant material.

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另一种是正常的干酪根热降解成熟原油。The other is normal mature crude oil from the thermal degradation of kerogen.

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。Natural gas is not only originated from kerogen cracking, but also from oil cracking.

生油母质干酪根是石油地质工作研究的重要对象。Oil-generating Parent material kerogen is the important target in petroleum geology study.

探讨了用X光衍射技术，测定干酪根芳香度的方法。The method for determination the aromatic degree of kerogen by X-ray diffraction was discussed.

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。Sapropelic gas could be derived from the cracking of both sapropelic kerogen and sapropelic crude oil.

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这些无机物的消除程度是用剩馀油母质的灰分含量测定的。The efficiency of the elimination of such minerals is measured by the ash content of the residual kerogen.

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。Generation of hydrocarbon from kerogen is one of important genetic types of abnormal pressure in source rock.

对干酪根演化史的恢复建议使用演化指数法为好。Thermalalteration index is a better way which was suggested that the recovering evolution history of kerogen.

该区有机质类型以腐泥型占绝对优势，且烃源岩整体处在成熟热演化阶段。The kerogen type of organic matter is predominantly sapropelic and evolution of source rock is during mature stage.

本文利用固定床反应器对干酪根进行加氢催化热解，提取干酪根中共价键结合的生物标志化合物。Fix-bed reactor was used to pyrolysis of kerogens to release the biomarker from kerogen by covalented bond cracking.

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盆地构造活动和火山作用可以促进干酪根的成烃转化。Tectonic activities and volcanism in the basin have an influence on hydrocarbon generation of kerogen and its change.

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。A new type of kerogen automatic preparation instrument can automatically operate the whole process of kerogen preparation.

本模拟实验主要对华北上元古界下马岭组页岩干酪根的热演化特征和规律进行研究。A simulation experiment was made on kerogen from shales in the lower Xiamalin Formation of the Proterozoic in North China.

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。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。Whole rock analysis and kerogen analysis are two analytical methods of studying hydrocarbon source rock in organic petrology.

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而长链脂肪酸盐由于难溶，在目前的有机地球化学处理过程中，它们主要和干酪根混在一起，少量的进入沥青质组分中。As their insolubility in organic solvents, long chain fatty acid salts mainly stay with Kerogen and few enter asphaltene fraction.

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 kinetic models commonly used are proposed that the reactions of hydrocarbon generation from kerogen are parallel and independent.

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 element composition and mature of kerogen is an important distinguish mark between great and small scale carlintype gold deposits.