Identification of Micro Fractures in Cretaceous Bioclastic Limestone in Iraq and Its Influence on Development of Reservoirs

Genjiu Wang, D. Hu, Qianyao Li
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Abstract

It is generally believed that Cretaceous bioclastic limestone in Mesopotamia basin in central and southern Iraq is a typical porous reservoir with weak fracture development. Therefore, previous studies on the fracture of this kind of reservoir are rare. As a common seepage channel in carbonate rock, fracture has an important influence on single well productivity and waterflooding development of carbonate reservoir. Based on seismic, core and production data, this study analyzes the development characteristics of fractures from various aspects, and discusses the influence of fractures on water injection development of reservoirs. Through special processing of seismic data, it is found that there are a lot of micro fractures in Cretaceous bioclastic limestone reservoir. Most of these micro fractures are filled fractures without conductivity under the original reservoir conditions. However, with the further development of the reservoir, the reservoir pressure, oil-water movement, water injection and other conditions have changed, resulting in the original reservoir conditions of micro fractures with conductivity. The water cut of many production wells in the high part of reservoir rises sharply. In order to describe the three-dimensional spatial distribution of fractures, the core data is used to verify the seismic fracture distribution data volume. After the verification effect is satisfied, the three-dimensional fracture data volume is transformed into the geological model to establish the permeability field including fracture characteristics. The results of numerical simulation show that water mainly flows into the reservoir through high angle micro fractures. Fractures are identified by seismic and fracture model is established to effectively recognize the influence of micro fractures on water injection development in reservoir development process, which provides important guidance for oilfield development of Cretaceous bioclastic limestone reservoir in the central and southern Iraq fields.
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伊拉克白垩系生物碎屑灰岩微裂缝识别及其对储层发育的影响
一般认为,伊拉克中南部美索不达米亚盆地白垩系生物碎屑灰岩是一种典型的裂缝发育弱的多孔储层。因此,以往对此类储层裂缝的研究较少。裂缝作为碳酸盐岩中常见的渗流通道,对碳酸盐岩油藏单井产能和注水开发具有重要影响。根据地震、岩心和生产资料,从多个方面分析裂缝发育特征,探讨裂缝对储层注水开发的影响。通过对地震资料的特殊处理,发现白垩系生物碎屑灰岩储层中存在大量微裂缝。这些微裂缝多为原始储层条件下无导流能力的充填裂缝。但随着储层的进一步开发,储层压力、油水运动、注水等条件发生了变化,形成了具有导流性的微裂缝原有储层条件。油藏高段多口生产井含水率急剧上升。为了描述裂缝的三维空间分布,利用岩心数据对地震裂缝分布数据体进行了验证。验证效果满意后,将三维裂缝数据体转化为地质模型,建立含裂缝特征的渗透率场。数值模拟结果表明,水主要通过高角度微裂缝进入储层。通过地震识别裂缝,建立裂缝模型,有效识别储层开发过程中微裂缝对注水开发的影响,为伊拉克中南部白垩系生物碎屑灰岩储层的油田开发提供重要指导。
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