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.
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