涠西南凹陷流沙港组二段烃源岩有机相研究

    Organic facies of source rocks of the second member of Liushagang Formation in the Weixinan sag

    • 摘要: 流沙港组二段是涠西南凹陷烃源岩发育的主要层位,对流沙港组二段烃源岩有机相的研究具有重要的意义。本文综合沉积环境、地球化学特征和生源构成等方面的分析,将流沙港组二段烃源岩划分为中深湖藻源母质相、中深湖混源母质相、滨浅湖混源母质相和扇三角洲混源母质相等四种类型有机相。其中中深湖藻源母质相分布广,有机质丰度高,有机质类型为Ⅰ-Ⅱ1型,厚度大,是涠西南凹陷的主力烃源岩,对油气的贡献最大;滨浅湖混源母质相分布也较广,有机质丰度较高,有机质类型主要为Ⅱ1-Ⅱ2型,厚度也较大,是涠西南凹陷的主要烃源岩。

       

      Abstract: JZ)The second member of Liushagang formation is the principal layer of source rocks in Weixinan sag,it is very important to research into the organic facies of source rocks of the second member of Liushagang formation.According to the analysis of sedimentary environment、geochemical characteristics and biological sources,the source rocks of the second member of Liushagang formation in Weixinan sag is divided into middle-deep lake algal source organic facies、middle-deep lake commix source organic facies、littoral and shallow lake commix source organic facies and fan delta commix source organic facies.The middle-deep lake algal source organic facies,widely and thickly distributed,rich in organic matter,with kerogen type of Ⅰ-Ⅱ1,is the main source rock of the Weixinan sag,and makes great contribution to oil and gas accumulation;Littoral and shallow lake commix source organic facies,widely and thickly distributed,rich in organic matter,with kerogen type of Ⅱ1-Ⅱ2,is the major source rock of the Weixinan sag.

       

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