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'LOSCS' lateral offset stacked channel simulations: Towards geometrical modelling of turbidite elementary channels

机译:“ LOSCS”横向偏移堆积通道模拟:浊积基本通道的几何建模

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Turbidite hydrocarbon reservoirs are complex features, that need to be described in detail and represented as clearly as possible. The morphology and internal distribution of elementary distributary channels are dependent on depositional settings, leading to diverse arrangements at different scales. Reservoir modelling usually requires a description of sedimentary heterogeneity on a scale smaller than that given by seismic resolution. This is because seismic data only display the outside geometry of their lateral stack, i.e. a turbidite fairway. Complexes of Laterally Offset Stacked Turbidite Channels (LOSCs) also require a description based on the scales of individual channel bodies. The most common representation of channels in a fairway is by stochastic object modelling; i.e. populating the observed fairway with realistic forms representing individual channels, but with no established consistency between the individual channels. On the other hand, one essential characteristic of LOSCs is that it evolves by progressive migration laterally and/or downdip. Stochastic object modelling provides an inadequate representation of this progressive evolution, and consequently, a poor rendering of the heterogeneity distribution in the reservoir. The method we propose consists of defining a realistic succession of individual channels that can accurately build the fairway observed on seismic. 'Realism' is defined using criteria from the shape of individual channels, and based on the amount of displacement necessary between successive episodes. Depending on seismic resolution, the system can be constrained by one or several positions of individual channels (the most recent position of the channel is often filled with shale, therefore visible on seismic and usable as a control point). The final result is a deterministic succession of channels laterally stacked to build the seismically observed envelope. Even with no calibration, the resulting architecture respects the general 'texture' of the complex and provides a better simulation of flow pathways than that achieved by random object modelling.
机译:浊石碳氢化合物储层具有复杂的特征,需要对其进行详细描述并尽可能清楚地表示。基本分配通道的形态和内部分布取决于沉积环境,从而导致不同规模的不同排列。油藏建模通常需要描述沉积异质性,其规模要小于地震分辨率给出的尺度。这是因为地震数据仅显示了其横向叠层的外部几何形状,即浊度球道。横向偏移堆叠浊度通道(LOSC)的复合体也需要根据单个通道体的规模进行描述。球道中最常见的通道表示是随机对象建模。即,以代表各个渠道的逼真的形式填充观察到的球道,但各个渠道之间没有确定的一致性。另一方面,LOSC的一个基本特征是它通过侧向逐渐迁移和/或下倾而演化。随机对象建模不足以表示这种渐进的演化,因此,储层中非均质性分布的绘制效果较差。我们建议的方法包括定义实际的单个通道序列,这些通道可以准确地建立地震观测中的航道。 “现实主义”是根据各个频道的形状以及连续剧集之间必要的位移量来定义的。根据地震分辨率,系统可能受到单个通道的一个或几个位置的约束(通道的最新位置经常充满页岩,因此在地震中可见并可用作控制点)。最终结果是横向堆叠以建立地震观测包络线的确定性连续通道。即使不进行校准,所得到的体系结构仍会遵循复杂系统的一般“纹理”,并且比通过随机对象建模获得的流路仿真效果更好。

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