首页> 外文会议>SPE Annual Technical Conference and Exhibition >Genesis of High Permeable Thief-zones and Integrated Reservoir Modeling of Intense Heterogeneous Reef-flat Carbonates: A Case Study for the Mishrif Formation of the Rumaila Oilfield, Iraq
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Genesis of High Permeable Thief-zones and Integrated Reservoir Modeling of Intense Heterogeneous Reef-flat Carbonates: A Case Study for the Mishrif Formation of the Rumaila Oilfield, Iraq

机译:高渗透性小区区的成因及强度异质珊瑚礁碳酸盐的集成储层模型 - 以伊拉克韩国韩国南方芦苇的Mishrif形成为例

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The super-giant Rumaila oilfield, with siliciclastic and carbonate reservoirs, has been developed for nearly 70 years. However, the Mishrif carbonates, which account for nearly half of Rumaila's reserves, could not be mass developed, as the current recovery rate is only 6%. One of the complexities is due to the presence of thin layers with abnormally high permeability, called thief-zones, which make reservoirs extremely heterogeneous and injection water breakthrough very early. Therefore, it is necessary to decipher the reservoir genesis and complicated architectures by genetic analysis, reservoir characterization and modeling for Mishrif's efficient development. Based on key flooding and erosion surfaces, sedimentary cycles in lithofacies and petrophysical responses, stratigraphy correlations and seismic strata stacking configurations, the fine isochronal stratigraphy framework of the Mishrif Formation has been constructed. Then, the genetic processes of lithofacies differentiation, reservoir distributions and properties, and thief-zones in response to palaeotopography and relative sea-level changes are analyzed synthetically in lithofacies, well-log sections, dynamic data and layer models from geological seismic units interpreted. According to petrophysics detection and reservoir genesis, the thief-zone distribution model is acquired. Subsequently, constrained by genetic conditions, 3D-gridding porosity model and double medium permeability model are constructed by simulation and integrated understanding of intricate architectures and permeability from cores and dynamic data. This paper demonstrates: 1) The Mishrif Formation can be divided genetically into six zones, from Zone Z1 to Z6; 2) The palaeotopography and relative sea-level changes control reef-flat deposition and differentiation so that the thick, coarse and clean lithofacies are usually distributed on upper parts of reef- flat build-ups but become finer in lower-side places. Furthermore, the Z1 thickness has important influences on Z1 and subsequent depositions; 3) Thief zones are not stress fractures, but rather erosion and leaching surfaces developed on top of reef-flat buildups in coarse lithofacies due to relative sea-level fluctuations; 4) The porosity models demonstrate high porosity (30-18%) in relative coarse lithofacies of reef-flat buildups, and reflect genesis of depositional energy environments by porosity distributions; 5)The permeability model has revealed reservoir intense heterogeneity (0.01- 4000mD), in which, the extremely high (>1000 mD) reservoirs, the thin thief-zones, are distributed mostly with lateral extension of 250-2300 m. The extremely- high, high and low reservoirs comprise complicated reservoir architectures which can at least be divided into three scenarios for reservoir development, in which the development of thief-zones in injectors should be paid more attention to designing perforation intervals because of possibly influences of extremely high permeable thief-zones. The methodology and results in this paper provide crucial references for the development of Rumaila oilfield and similar heterogeneous carbonate reservoirs.
机译:具有硅砾和碳酸盐储层的超巨型Rumaila油田已开发出近70年。然而,Mishrif碳酸碳酸盐,占Rumaila储备的近一半,不能批量发展,因为目前的恢复率仅为6%。其中一种复杂性是由于存在具有异常高渗透性的薄层,称为窃贼区,这使得储层非常不均匀和注入水突破。因此,有必要通过遗传分析,储层表征和模型来破译储层成因和复杂的架构,以便MishRIF的有效发展。基于关键洪水和侵蚀表面,岩石遗传沉积循环和岩石物理响应,地层相关性和地震层堆叠配置,已经构建了MishRIF形成的细胞型层状框架。然后,在岩石静脉曲张,井对数截面,从地质地震单元解释的地质地震单元的动态数据和层模型中,分析了岩石缩合分化,储存分布和性质和盗贼区的遗传过程,以及相对海平改变的临时分析。根据岩石物理检测和储层创世纪,获取了小区区分布模型。随后,通过遗传条件,3D集成孔隙度模型和双级渗透性模型通过模拟和综合了解复杂的架构和来自核心和动态数据的渗透性构成。本文表现出:1)MishRIF地层可以从区域Z1至Z6遗传地分为六个区域; 2)古代复印术和相对海平面的变化控制珊瑚扁平沉积和分化,使厚,粗糙和清洁的岩型通常分布在Reef-Flats-Ups的上部,但在较低的地方变得更精细。此外,Z1厚度对Z1和随后的沉积具有重要影响; 3)小偷区域不是压力骨折,而是由于相对海平波动而在粗岩缺陷的珊瑚礁堆上开发的腐蚀和浸出表面; 4)孔隙率模型在Reef-Flatsups的相对粗岩型中表现出高孔隙率(30-18%),并通过孔隙分布反射沉积能量环境的起源; 5)渗透性模型揭示了储层强烈异质性(0.01-4000MD),其中,极高(> 1000md)储存器,薄的小偷区,主要用250-2300米的横向延伸分布。极高,高储层的水库包括复杂的水库架构,其至少可以分为三个储层开发场景,其中由于可能的影响,应该更加关注设计的窃贼区的三个情景极高的渗透性窃贼区。本文的方法和结果为Rumaila油田和类似的异质碳酸盐储层提供了关键的参考。

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