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Predicting the distribution of potential reservoir facies through sedimentological comparison of modern depositional analogs -A case of fluvial deltaic sandstone reservoirs in Eastern Venezuela-

机译:通过现代沉积类似物的沉积学比较来预测潜在水库相的分布-a委内瑞拉的河流德国砂岩储层的情况 -

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摘要

The Guarico 13 field is located in the western Greater Oficina area, Eastern Venezuela basin. and consists of a large number of hydrocarbon accumulation in sandstones deposited in a coastal-plain environment. Trapping mechanisms for exploration opportunities in the study area combine structural faulting and stratigraphic pinch out. Individual reservoir thickness is normally 20ft or less and therefore it is hard to detect the reservoir distribution and the limits of hydrocarbon trapping area by using seismic data even if a seismic inversion process is carried out. Although the size of each individual reservoir is small. multiple reservoir sections were observed in each well and the sum of these reserves will be worth developing. It is very important to predict the potential reservoir facies to increase oil production and to discover additional new reservoirs in this kind of sandstones deposited in a fluvial-deltaic system. The high-resolution stratigraphy in the area was achieved by correlating all the lignite beds that occur between the major marine and lacustrine flooding surfaces. Then the core intersections. log character. borehole image logs and palynology were utilized to estimate the depositional environment of each hydrocarbon-bearing stratigraphic unit. After this environmental analysis. modern analogs and a geological model were applied to predict the reservoir facies and its extent. In this report. the authors demonstrate two case studies of estimating the reservoir distribution ; one uses a template model of a major bed-Ioad fluvial system with crevasse splay sands on interfluve area, and another employs a crosscutting tidal inlet and associated ebb'tidal delta system as an analog. This sort of approach that uses modern analogs as templates is worth applying to predict the potential distribution of reservoir sandstone if 3D seismic is not available or can not detect reservoir extent.
机译:Guarico 13田地位于东委内瑞拉盆地东部大区。并且包括在沿海普通环境中沉积的砂岩中的大量碳氢化合物积累。研究区勘探机遇的捕获机制结合了结构断层和地层夹出来。单个贮存器厚度通常为20英尺或更小,因此即使进行地震反转过程也很难通过使用地震数据来检测储存器分布和烃捕获区域的限制。虽然每个单独的水库的大小很小。在每个井中观察到多个水库部分,这些储备的总和将值得开发。预测潜在的水库相片,增加石油生产并在这种沉积在氟尿 - 丹特系统中探索额外的新水库是非常重要的。该地区的高分辨率地层通过与主要海洋和湖泊洪水泛滥表面之间发生的所有褐煤床相关来实现。然后是核心交叉路口。日志字符。使用钻孔图像日志和椎相论来估计每个含烃地层单元的沉积环境。在这种环境分析之后。应用现代模拟和地质模型来预测水库各界及其程度。在本报告中。作者展示了估计储层分布的两种情况研究;一体地使用带有Crefluve地区的裂隙Splay Sands的主要床的模板模型,另一个使用横切潮气入口和相关的EBB'tidal Delta系统作为模拟。使用现代模拟作为模板的这种方法值得申请预测如果3D地震不可用或无法检测到储层范围,则申请储层砂岩的潜在分布。

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