首页> 外文会议>ICEESD 2011;International Conference on Energy, Environment and Sustainable Development >Controls of Short-Term Base-Level Cycle on Macroscopic Heterogeneity of Reservoir: a case study of the major oil layer of Liuzan Oilfield in Nanpu Sag
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Controls of Short-Term Base-Level Cycle on Macroscopic Heterogeneity of Reservoir: a case study of the major oil layer of Liuzan Oilfield in Nanpu Sag

机译:对储层宏观异质性的短期基础级周期的控制 - 以南浦凹陷脉冲油田大型油层的案例研究

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Based on the depositional model and characteristics of fan delta, the short-term base-level cycle of the third submember of the third member of Shahejie Formation (Es_3~3) in North region major oil layer of Liuzan Oilfield of Nanpu Sag is divided into three basic categories applying high-resolution sequence stratigraphy with the reference to core and logging data, namely, deepening-upward asymmetrical type, shallowing-upward asymmetrical type and symmetrical type. Different variation models for macroscopic heterogeneity of reservoir belonging to different categories of short-term base-level cycle were established in this paper; it was further pointed out that the changes of base-level and the ancient landform were major factors controlling the characteristic discrepancy of macroscopic heterogeneity of reservoir. In fan delta plain area, the ancient landform is smooth. Deepening-upward asymmetrical cycle is mainly composed of braided river sand body, and the changes of base-level exert little control on porosity with significant control on permeability. At the delta front slope, the landform becomes steep. Deepening-upward asymmetrical cycle is mainly composed of underwater distributary channel with genetic mechanism of gravity flow. The vertical variations of porosity and permeability inside the cycle are rather complicated. Since the physical properties are mainly manifested as the control on autogenic cycle, they do not directly influence the changes of base level.
机译:基于风扇三角洲的沉积模型和特点,南部南浦芽南部油田的北部地区三角形(ES_3〜3)第三次成员的第三次成员的短期基础周期循环分为三个基本类别应用高分辨率序列地层参考核心和测井数据,即深化向上不对称类型,浅浅的不对称类型和对称类型。本文建立了属于不同类别的短期基础级循环的水库宏观异质性的不同变化模型;进一步指出,基础水平和古代地貌的变化是控制水库宏观异质性特征差异的主要因素。在粉丝三角洲平原地区,古代地貌流畅。深化上向上的不对称周期主要由编织河砂体组成,基础级的变化对渗透性有重大控制的孔隙率施加很少。在三角洲前坡,地貌变得陡峭。深化向上的不对称周期主要由水下分配通道组成,具有重力流动的遗传机制。循环内部孔隙率和渗透率的垂直变化是相当复杂的。由于物理性质主要表现为自动循环对控制,因此它们不会直接影响基础水平的变化。

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