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An in-depth analysis of reservoir architecture of underwater distributary channel sand bodies in a river dominated delta: A case study of T51 Block, Fuyu Oilfield, Jilin

机译:河流主导三角洲水下分流河道砂体储层构造的深度分析-以吉林扶余油田T51区块为例

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Guided by the concept of “model fitting, dynamic validation”, and based on the data of 10 coring wells, 257 logging wells, and the production performance in the dense spacing area during the past ten years, the underwater distributary channel sand reservoir in K1q4of T51 Block, Fuyu Oilfield, Songliao Basin, was analyzed to examine the spatial distribution and identification marks of the architectures within the reservoir. Results indicated that the single channel sand body is 300–500 m wide and can be identified by such marks as inter-channel sediments, sand elevation difference between wells, difference of channel sand thickness, and “thick-thin-thick” sands association; the dip angle of the fourth-order interface is 0°–2°. Besides, the logging response characteristics and identification method of single channel sand bodies and their interior accreted bodies were defined for the reservoir. A 3D architecture model is established for the underwater distributary channel reservoir in the study area, providing a quantitative and reliable geological model for analysis of underwater distributary channel sands in the whole area.
机译:在“模型拟合,动态验证”的概念指导下,以10口取水井,257口测井的数据以及近十年来在密集空间区域的生产性能为基础,K1q4的水下分流河道砂岩储层对松辽盆地扶余油田T51区块进行了分析,研究了储层内部结构的空间分布和识别标志。结果表明,单道砂体的宽度为300-500 m,可以通过道间沉积物,井间砂高差,通道砂厚度差和“厚-薄-厚”砂组合等标志来识别。四阶界面的倾角为0°–2°。定义了储层单道砂体及其内部增生体的测井响应特征和识别方法。为研究区域的水下分水道水库建立了3D体系结构模型,为分析整个区域的水下分水道砂提供了定量和可靠的地质模型。

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