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Charging of oil fields surrounding the Shaleitian uplift from multiple source rock intervals and generative kitchens, Bohai Bay basin, China

机译:渤海湾盆地多源岩层段和增生厨房对沙勒田隆起周围的油田充注

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This paper discusses origin and charging directions of oil fields on the Shaleitian Uplift, Bohai Bay basin. The Shaleitian Uplift is a footwall uplift surrounded by three sags containing mature source rocks. The origins of the four oil fields on the Shaleitian Uplift, both in terms of source rock intervals and in terms of generative kitchens, were studied using biomarker distributions for 61 source rock samples and 27 oil samples. Hierarchical cluster analysis using 12 parameters known to be effective indicators of organic matter input and/or depositional conditions allowed the identification of six oil types or classes. These six oil classes could then be linked to three distinct source rock intervals ranging in age from 43.0 Ma to 30.3 Ma. The third member (43.0-38.0 Ma in age) and first member (35.8-32.8 Ma) of the Eocene Shahejie Formation, and the third member of the Oligocene Dongying Formation (32.8-30.3 Ma) each sourced one class of oil. The other three classes represent mixtures of oil generated from multiple source rock intervals. Traps on the Shaleitian Uplift were charged in the east by oil generated from the Eocene Shahejie Formation in the Bozhong Sag, in the southeast by oil generated from the Eocene Shahejie and then Oligocene Dongying formations in the southwestern part of the Bozhong Sag and/or in the eastern part of the Shanan Sag, and in the southwest by oil generated from the Eocene Shahejie Formation in the western part of the Shanan Sag. The estimated migration distances range from less than 5 km to about 20 km. The compositional heterogeneity within fields and multiple-parameter comparisons between oils from nearby wells in different fields have proven to be a powerful tool to determine the in-filling histories of oil fields in cases where multiple source rock intervals and multiple generative kitchens exist.
机译:本文探讨了渤海湾盆地沙勒田隆起的油田成因和充注方向。 Shaleitian隆起是一种底盘隆起,周围是三个凹陷,其中包含成熟的烃源岩。利用生物标志物分布对61个烃源岩样品和27个石油样品进行了研究,研究了Shaleitian隆起的4个油田的起源,无论是在烃源岩层段方面还是在生成厨房方面。使用已知为有机物输入和/或沉积条件的有效指标的12个参数进行的层次聚类分析可以识别出六种油类或类别。然后可以将这六个油类与年龄从43.0 Ma到30.3 Ma的三个不同的烃源岩层段联系起来。始新世沙河街组的第三组(年龄为43.0-38.0 Ma)和第一组(35.8-32.8 Ma),以及渐新世东营组的第三组(32.8-30.3 Ma)均采出一类油。其他三个类别表示从多个烃源岩层段产生的油的混合物。东部由渤中凹陷始新统始新统沙河街组产生的油充填,东南由先始始新统Shahejie始生的油,然后由渤中凹陷西南部和/或中新统东营组充填。 Shanan凹陷西部的始新世沙河街组所产生的石油在Shanan凹陷的东部和西南部。估计的迁移距离范围从不到5公里到大约20公里。事实证明,在存在多个烃源岩层段和多个生成厨房的情况下,油田内部的成分异质性和来自不同油田附近井的油之间的多参数比较是确定油田填充历史的有力工具。

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