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Overview of Depositional and Diagenetic Impacts on Reservoir Characterization, Karachaganak Field, Kazakhstan

机译:对储层特征,卡扎卡南省,哈萨克斯坦的储层和成岩作用概述

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Karachaganak Field is a giant gas-condensate reservoir located in north-western Kazakhstan. The reservoir is composed of an isolated carbonate build-up of Carboniferous - Early Permian age, located on the northern edge of the Pri-Caspian Basin. The reservoir is overlain by three thick salt domes which were formed by the movement of an evaporitic sequence deposited at the end of Early-Permian. This salt tectonics has locally affected the seismic image of the reservoir and consequently makes seismic interpretation challenging. A high fold and wide-azimuth 3D seismic volume has been acquired over Karachaganak. Preliminary migrations of this new seismic volume have improved resolution of the reservoir geometry and facies. The Karachaganak carbonate reservoir is characterized by both slope and platform depositional systems, and the reservoir has undergone significant diagenetic alteration. Diagenesis has altered the original depositional rock fabric, pore and pore throat geometry. Critical reservoir properties such as porosity, permeability and irreducible water saturation at Karachaganak are influenced by of both depositional and diagenetic processes. The degree of diagenetic alteration of Karachaganak is greater than some other analogous carbonate reservoirs in the Pri-Caspian basin. This paper discusses the current reservoir model for the post-Tula Carboniferous deposits, which is based on a synthesis of understanding of the depositional and diagenetic processes at Karachaganak. The current reservoir model incorporates the results from recently drilled wells, recent interpretations of 3D seismic data and well tests. The resulting dynamic model has a good history match to observed well performance, and provides a basis for field development decisions. Karachaganak Petroleum Operating (KPO) joint-venture is conducting additional studies of the field deposition and diagenesis to provide new insights into the complex geological history of the field to improve reservoir characterization and reservoir management activities.
机译:Karachaganak领域是位于哈萨克斯坦西北部的巨型气凝矿水库。水库由位于Pri-Caspian盆地北部边缘的孤立的碳酸盐覆盖物的孤立的碳酸盐积累组成。储存器由三个厚的盐圆形覆盖,该圆形圆形圆顶由蒸发在早期沉积在早期二叠套末端的蒸发序列的运动形成。这种盐构造局部影响了水库的地震形象,从而使地震解释具有挑战性。通过卡拉丘纳克获得了高折叠和宽方向的3D地震体积。这种新地震卷的初步迁移具有改进的水库几何形状和相片的分辨率。卡拉达替纳克碳酸盐贮存器的特点是坡度和平台沉积系统,贮存器经历了显着的成岩变化。成岩作用改变了原始的沉积岩石织物,孔和孔喉几何形状。 Karachaganak在卡拉丘纳克的孔隙度,渗透率和不可缩续的水饱和度的关键储层性质受到沉积和成岩工艺的影响。卡拉丘纳克的成岩变化程度大于PRI-CASPIAN盆地中的其他一些类似的碳酸盐储层。本文讨论了后杜拉石油沉积物的现有储层模型,其基于对卡拉丘纳克的沉积和成岩性过程的理解合成。目前的储层模型包含最近钻孔井的结果,最近对3D地震数据和井测试的解释。由此产生的动态模型具有良好的历史匹配,以观察到井的性能,为现场开发决策提供基础。 Karachaganak石油运营(KPO)合资企业正在进行近期研究田间沉积和成岩作用,以便为该领域的复杂地质史提供新的见解,以改善水库特征和水库管理活动。

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