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.
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.
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。
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.
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。
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.
天然气乙烷碳同位素与各层系烃源岩干酪根碳同位素值对比结果揭示普光气田天然气主要来自二叠系烃源层。
The carbon isotope correlation between ethane in the natural gases and source rock kerogens shows that the gases in the reservoirs were mainly derived from Permian strata.
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。
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。
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.
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