首页> 外文期刊>Open Journal of Geology >Research on Thin Layer Structure Identification and Sedimentary Facies of Middle and Deep Layers Based on Reflection Coefficient Inversion—By Taking Dongying Formation of CFD Oilfield in Bohai Offshore as an Example
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Research on Thin Layer Structure Identification and Sedimentary Facies of Middle and Deep Layers Based on Reflection Coefficient Inversion—By Taking Dongying Formation of CFD Oilfield in Bohai Offshore as an Example

机译:基于反射系数反演的中层层薄层结构识别和沉积相研究 - 以渤海海上粮食植信合卖油田东营形成为例

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The sand layer B of Dongying Formation of CFD oilfield in Bohai offshore belongs to the middle deep layer of buried hill overlap deposit. Its reservoir distribution has the characteristics of large burial depth, thin thickness and rapidly lateral change. Because of low resolution of seismic data and overlying sand layer. It is difficult to identify and interpret the structure of sand layer accurately. The uncertainty of structure and reservoir restricts the fine development of B sand layer. In order to identify the top surface of reservoir effectively. The seismic data are processed by using the reflection coefficient inversion method. The results show that the inversion resolution of reflection coefficient is significantly higher than that of original data. The top surface of sand layer B and its overlying sand layer can be well identified and traced. Carrying out structural interpretation of B sand layer based on reflection coefficient inversion data and the microstructure and the formation tip extinction point are implemented. Based on the constraint of new interpretation level, the sedimentary facies plane distribution of B sand layer is described and make prediction of dominant reservoir development area in detail combining with sedimentary paleogeomorphology, along layer attribute section and limited drilling data. The research shows that the study area is mainly from the northwest material sources, the slope belt in the northwest is close to the lake shoreline with a gentle slope and shallow water depositional environment, which is located on the main transport and deposition channels. The shallow water gentle slope landform is suitable for forming large-area sand bar deposition, mainly composed of underwater distributary channel and debouch bars facies, which is the dominant reservoir development area. The research conclusion guides the deployment and implementation of the development well location effectively.
机译:渤海海上CFD油田的东营形成的沙层B属于埋藏山脉的中间深层沉积。其储层分布具有大的埋藏深度,薄厚度薄,横向变化的特点。由于地震数据和覆盖砂层的分辨率低。很难精确识别和解释砂层的结构。结构和水库的不确定性限制了B砂层的细弱。为了有效地识别储层的顶部表面。通过使用反射系数反演方法处理地震数据。结果表明,反射系数的反转分辨率显着高于原始数据的反转分辨率。砂层B的顶表面及其覆盖的砂层可以很好地识别和追踪。实施基于反射系数反演数据的B砂层的结构解释,并实现了微观结构和形成尖端消光点。基于新的解释水平的约束,描述了B砂层的沉积相平面分布,并详细描述了与沉积古正像术的沉积储层开发区域的预测,沿着层属性部分和有限的钻探数据。该研究表明,该研究领域主要来自西北物料来源,西北部的坡带靠近湖岸线,较轻的斜坡和浅水沉积环境,位于主运输和沉积通道上。浅水平缓坡地地貌适用于形成大面积砂杆沉积,主要由水下分销渠道和挖掘杆相板组成,这是主要的水库开发区。研究结论有效地指导了发展良好位置的部署和实施。

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