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首页> 外文期刊>Journal of African Earth Sciences >Facies and petrophysical modeling of the Upper Bahariya Member in Abu Gharadig oil and gas field, north Western Desert, Egypt
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Facies and petrophysical modeling of the Upper Bahariya Member in Abu Gharadig oil and gas field, north Western Desert, Egypt

机译:埃及西北沙漠北部阿布加拉迪格油气田的上巴哈里亚岩相和岩石物理模拟

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摘要

The Upper Bahariya Member represents an argillaceous sandstone reservoir and it is one the Late Cretaceous units. There is a need for understanding the detailed fades and petrophysics of this member and identifying whether its petrophysical parameters are related to the fades changes or the present structures. Therefore, the present study aims at determining the fades and petrophysical characteristics of the Upper Bahariya Member and their distribution in the Abu Gharadig field. This field is located in the central portion of Abu Gharadig basin in the northern part of the Western Desert of Egypt. The available data for the present study includes four digital well logs, twenty 2D seismic sections and a checkshot survey. This is achieved through building the 3D facies and petrophysical models using Petrel (TM) Schlumberger Modeling software. These models were built on a predefined 3D stratigraphic and structural framework. The interpreted lithology of the Upper Bahariya Member is represented by sandstone cemented by argillaceous and/or calcareous materials, siltstone, shale and minor limestone inter-beds. A new lithofacies subdivision for the Upper Bahariya is introduced in the present study through the study area. This subdivision is represented by three lithofacies (an upper shale-silt-carbonate lithofacies, a middle sand-silt lithofacies and a lower shale-silt lithofacies). The Upper Bahariya Member is evaluated as a good quality reservoir and it exhibits rapid variations in the conditions of deposition, from continental fluvial to marine passing through the tidal flood plain conditions. The sandstone source is mainly from the southeast and southwest directions. The vertical and lateral changes of the different petrophysical parameters are directly related to vertical and lateral facies changes.
机译:上巴哈里亚岩体是泥质砂岩储集层,是白垩纪晚期单元。需要了解该成员的详细的衰变和岩石物理学,并确定其岩石物理参数是否与衰变变化或当前结构有关。因此,本研究旨在确定上巴哈里亚成员的淡化和岩石物理特征及其在阿布加拉迪格地区的分布。该油田位于埃及西部沙漠北部的阿布加拉迪格盆地的中部。本研究的可用数据包括四个数字测井记录,二十个2D地震剖面和一个抽查调查。这是通过使用Petrel(TM)Schlumberger建模软件构建3D相和岩石物理模型来实现的。这些模型建立在预定义的3D地层和结构框架上。上巴哈里亚岩层的解释性岩性表现为以泥质和/或钙质物质胶结的砂岩,粉砂岩,页岩和少量石灰岩夹层。通过研究区域,本研究引入了上巴哈里亚的新岩相细分。该细分由三个岩相(上页岩-粉状碳酸盐岩相,中层砂-粉状岩相和下页岩-粉状岩相)表示。上巴哈里亚成员被认为是优质储层,其沉积条件从大陆河床到经过潮汐洪泛平原条件的海洋,其沉积条件都有快速变化。砂岩源主要来自东南和西南方向。不同岩石物理参数的垂直和横向变化与垂直和横向相变化直接相关。

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