川中地区侏罗系烃源岩和原油中三环萜烷分布特征及指示意义

    DISTRIBUTION AND INDICATION OF TRICYCLIC TERPANE IN JURASSIC SOURCE ROCKS AND CRUDE OIL IN CENTRAL SICHUAN BASIN

    • 摘要: 借助气相色谱-质谱技术, 通过对川中地区侏罗系大安寨段烃源岩及原油样品的系统地球化学分析, 揭示了生物标志物中三环萜烷系列的分布特征, 并探讨了其对于沉积环境和生物来源的指示意义. 结果表明: 大安寨段烃源岩及原油姥植比Pr/Ph中等, C19-C26三环萜烷呈现C21优势. C19+20和C23的相对百分含量较低, C24TeT/C26TT值大于1, 指示大安寨段沉积时期水体较浅, 生源构成以菌藻生源为主, 兼有丰富的高等植物生源的混源输入, 形成于弱还原的淡水湖相环境.

       

      Abstract: The distribution characteristics of tricyclic terpenes in biomarkers and their indicative significance for sedimentary environment and biological sources are discussed through the systematic geochemical analysis of source rocks and crude oil samples from Jurassic Da'anzhai Member in central Sichuan Basin by gas chromatography-mass spectrometry (GC-MS). The results show that the Pr/Ph ratios of source rocks and crude oil are medium level, with C19-C26 tricyclic terpenes showing the dominance of C21, low relative percentages of C19+20 and C23 contents, and C24TeT/C26TT value greater than 1, indicating that the water was shallow during the sedimentary period of Da'anzhai Member, and the biogenesis was mainly bacteria and algae, with rich mixed-source input of higher plants, which was formed in the weak reduction environment of freshwater lake facies.

       

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