首页> 外文会议>International Field Exploration and Development Conference >Evolution Process Characteristics of and Differential Enrichment of Oil and Gas in Deep Water Gravity Flow Sandstone Taking the MD Oilfield of the Eocene Shahejie Formation in the Huanghua Depression of Beidagang as an Example
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Evolution Process Characteristics of and Differential Enrichment of Oil and Gas in Deep Water Gravity Flow Sandstone Taking the MD Oilfield of the Eocene Shahejie Formation in the Huanghua Depression of Beidagang as an Example

机译:深水重力流动砂岩中石油和气体鉴别富集的进化过程特征,以北京黄花坳陷为例,为麦田坳陷MD油田为例

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Based on new theory of deep water sandstone,the sedimentary process of the gravity flow sandstone of the Shahejie Formation in the Huanghua depression was divided into four sandstone zones of genetic types in this work:sliding,slumping,sandy debris flow and turbidity flow by comparing sedimentary structures of typical cores,variation of grain sequence,difference of the reservoir physical properties,lithologic vertical combination sequences,and diagrams of well logging facies.The geometry and contact relationship of sandstones of different genesis were studied,and the evolution model of gravity flow sedimentation process was figured out.Combined with dynamic production data,the pattern of oil and gas differential enrichment was analyzed.Horizontally,the slump deposits are in the root segment of the downthrow block within a synsedimentary fault,and sandy clastic sediments are easily formed in the slope zones in front of the slump deposits.During the forward transport of the debris flows,the fluid gradually dilutes and transforms into turbid flows,which are distributed in the side and front of the debris flow.Vertically,there is a thin layer of turbidity deposit between the tops of the thick sandy debris flow with weakening energy,and the sandy debris flow can evolve into thin layers that develop between the turbid flows.Combined with dynamic production data,it is believed that the low-saturation reservoir with oil-bearing occurrence controlled by reservoir physical properties is likely to develop in the slope zone of sandy debris flows,and low-permeability reservoirs with no tectonic background is easily formed in the turbidity flow zone.For the first time,the logging facies diagrams of four genetic types of sandstones in deep water gravity flow were established,guiding the analysis of sedimentary process evolution models.In addition,the understanding of differential enrichment regularities of oil and gas points out the direction of sweet point evaluation and prediction.
机译:基于深水砂岩的新理论,黄花坳陷沙河街形成重力流砂岩的沉积过程分为四种遗传类型的砂岩区:滑动,坍塌,砂岩流动和浊度流动典型核心沉积结构,晶粒序列的变化,储层物理性质,岩性垂直组合序列和井井井晶体的图。研究了不同创世纪的砂岩的几何和接触关系,以及重力流动的演化模型沉淀过程被送出了动态生产数据,分析了石油和气体差异富集的模式。水平,坍落度沉积物在综合性故障内的滴管块的根部段中,砂质碎屑沉积物易于形成坍落度沉积物前面的斜坡区域。碎片流动的前向运输,流体逐渐稀释并转变成浑浊,它们分布在碎片流动的侧面和前面。较厚的砂质碎片流动之间存在薄薄的浊度沉积物,能量疲软,以及砂岩碎片流量可以发展成薄层,该层在浑浊的流动之间产生的动态生产数据,据信,通过储存器物理性质控制的低饱和贮存器可能在桑迪碎片流动的斜坡区中发展浊度流动区的低渗透储存器和无构造背景的低渗透储层建立了沉积物重力流动中的四种遗传类型的砂岩的测井相图,引导了沉积工艺演进模型的分析加法,对石油和天然气的差异富集规律的理解指出了甜点评估和预测的方向在。

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