THE SUBSURFACE GEOLOGY AND RESERVOIR CHARACTERISTICS OF THE UPPER BAHARIYA RESERVOIR IN THE HAYAT/YASSER OIL FIELD, NORTHWESTERN DESERT, EGYPT

A. Khadrah
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Abstract

The litho-stratigraphic cross sections, thickness variations and lithofacies of the Upper Bahariya reservoir (Upper Bahariya Member) are discussed to distinguish the shape, the extent of sedimentary basins and the environment of deposition. The studied Upper Bahariya reservoir shows that the Upper Bahariya Member top is coming higher at Yasser-06 well than the other three wells, which lies in the northeastern part of the study area. Furthermore, the maximum thickness of the Bahariya Formation occurs at Hayat-12, while the minimum thickness occurs at Hayat-17 well. The facies triangle lithologic model of the Upper Bahariya Member shows, the predominance of calcareous shale facies in most of the studied wells which change to shaley sand in the central part at Hayat-12 and Hayat-14 wells. These facies reflect a shallow marine environment grading from tidal-dominated estuarine channels to wave-dominated shoreline associating with lagoons or bays. The petrographic analysis shows that, there is a variation in the reservoir quality based on the detrital clay components and diagenetic processes.
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埃及西北部沙漠地区hayat / yasser油田上bahariya储层地下地质及储层特征
通过对上巴哈里亚储层(上巴哈里亚段)的岩性地层剖面、厚度变化和岩相特征的研究,对沉积盆地的形态、范围和沉积环境进行了区分。上巴哈里亚储层研究表明,位于研究区东北部的雅尔-06井上巴哈里亚段顶高高于其他3口井。此外,Bahariya组的最大厚度出现在Hayat-12井,而最小厚度出现在Hayat-17井。上巴哈里亚段三角相岩性模型表明,研究井大部分以钙质页岩相为主,中部在哈亚-12和哈亚-14井转变为泥质砂相。这些相反映了一个由潮汐主导的河口河道到波浪主导的与泻湖或海湾相结合的海岸线的浅海环境。岩石学分析表明,碎屑粘土组分和成岩作用对储层质量有一定影响。
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