首页> 外文期刊>Journal of Asian earth sciences >A comparative study of source rocks and soluble organic matter of four sags in the Jiyang Depression, Bohai Bay Basin, NE China
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A comparative study of source rocks and soluble organic matter of four sags in the Jiyang Depression, Bohai Bay Basin, NE China

机译:渤海湾盆地渤海湾盆地四个落下源岩和溶质有机物的比较研究

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The Jiyang Depression is a petroleum-rich basin in eastern China and has four petroleum sags: the Dongying, Zhanhua, Huimin and Chezhen Sags. However, the petroleum resources in the four sags differ greatly. We collected Rock-Eval pyrolysis and vitrinite reflectance (Ro) data for source rocks and the contents, group components and GC-MS data for soluble organic matter (SOM) to investigate the reasons for the hydrocarbon differences among the four sags. The results show that the source rock characteristics in the Jiyang Depression can be divided into two types: the type in the Dongying and Zhanhua Sags has greater abundances and better kinds of organic matter than the other type in the Chezhen and Huimin Sags. The Dongying and Zhanhua Sags correspondingly host higher SOM contents and more hydrocarbon components than the Chezhen and Huimin Sags. The evolutions of Ro in the Dongying Sag and the Zhanhua Sag are similar. However, the evolutions of SOM differ: the depth at which the SOM content and the relative content of saturates and resins substantially change in the Dongying Sag is shallower than that in the Zhanhua Sag. Additionally, the evolution of clay minerals corresponds well with the evolution of SOM, which indicates that the differences in clay minerals may cause the differences in the evolution of SOM. Therefore, the distribution in petroleum resource is jointly controlled by the source rock characteristics, thermal evolution and mineral evolution. Thus, organic-inorganic interaction should be a focus of the future research on hydrocarbon generation and petroleum resource evaluation.
机译:济阳坳陷是中国东部的石油丰富的盆地,拥有四个石油凹陷:东营,湛化,惠民和沉镇凹陷。然而,四个落下的石油资源很大。我们收集了源岩的岩石 - 醇热解和vitriinite反射率(RO)数据,用于可溶性有机物质(SOM)的源岩和内容物,组组分和GC-MS数据,以研究四个凹凸中烃差的原因。结果表明,济阳坳陷的源岩特征可分为两种类型:东营和湛化凹陷的类型有更多的丰富和更好的有机物质,而不是其他类型的横真和惠民凹陷。东营和湛化的落下相应地举办了索华更高的索收内容和更多的碳氢化合物组件,而不是横真和惠民凹陷。东营凹陷和湛化凹陷中的RO的演变是相似的。然而,SOM的演变不同:SOM含量和饱和物和树脂的相对含量在东营凹陷中的饱和含量大致变化的深度比Zhanhua凹陷在较浅的速度浅。另外,粘土矿物的演变与SOM的演化相吻合,这表明粘土矿物的差异可能导致SOM的演变差异。因此,石油资源的分布由源岩特性,热演化和矿物进化共同控制。因此,有机无机互动应成为未来烃生成和石油资源评估研究的重点。

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