首页> 外文期刊>Journal of Natural Gas Geoscience >Orgaofaices evolution of deep Es4 source rock in Baxian Sag, Jizhong Depression of Bohai Bay Basin and its significance, China
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Orgaofaices evolution of deep Es4 source rock in Baxian Sag, Jizhong Depression of Bohai Bay Basin and its significance, China

机译:Baxian凹陷,渤海湾盆地冀中坳陷的深度ES4烃源岩的演变及其意义及其意义

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The Es4 source rock is the primary source of hydrocarbon in deep reservoirs in the Baxian Sag, Jizhong Depression of Bohai Bay Basin, China, and its quantitative description is useful for understanding hydrocarbon generation and accumulation in the deep basin. The Es4 source rock contains organofacies C, D/E and F, with organofacies C having a thin thickness of less than 40 m and organofacies D/E having a thickness of 50 m and 250 m. The drilled Es4 source rock has a maximum RO of 1.27%, indicating that it is in the late oil window. The kinetic parameters for three organofacies source rock have been obtained from the simulation of gold tube pyrolysis. The result showed that organofacies C, D/E and F source rock entered into the mature level in sequence, but that at 150 °C, the organofacies C will be transformed to around 90% of their original state. For organofacies D/E and F, the hydrocarbon generation potential is still high, with condensate and wet gas dominating.
机译:ES4源岩是Baxian凹陷的深层烃源的主要来源,渤海湾盆地,渤海湾盆地的萧条凹陷及其定量描述可用于了解深盆地的碳氢化合物生成和积累。 ES4烃源岩含有有机碎裂的C,D / E和F,有机碎裂薄厚度小于40μm,厚度为50μm和250μm的有机原料d / e。 钻孔的ES4烃源岩的最大RO为1.27%,表明它位于后期油窗口。 从金管热解的模拟中获得了三种有机碎裂源岩的动力学参数。 结果表明,有机碎裂的C,D / E和F源岩按顺序进入成熟水平,但在150℃下,有机缩乳C将转化为其原始状态的约90%。 对于有机面物D / E和F,烃源潜力仍然高,凝结物和湿气体占据主导地位。

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