巴基斯坦印度河盆地中部始新世碳酸盐岩储层特征

Razib Asim Zeb, Muhammad Haziq Khan, Waqas Naseem, M. Awais, Hamza Zaheen, A. Khalid
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摘要

本文对巴基斯坦中部印度河盆地Qadirpur气田井侵始新统隋主灰岩(SML)进行了岩石物理分析。分析的SML岩石物性包括页岩体积、总孔隙度、有效孔隙度、含水饱和度、含烃饱和度和净产层厚度。研究结果表明,绥主灰岩储层具有可观的产油能力。岩石物理解释表明,研究的SML具有生产储层特征,平均(总孔隙度和有效孔隙度)在K-1层为15%,K-2层为15%,K-3层为17%,平均饱和烃含量为(70-100%),表明井内储层为纯饱和储层,K-1层页岩平均体积为23%,K2层为27%,K-3层为25%,表明储层为清洁储层。相模拟结果表明,研究的始新统组由洁净灰岩、泥质灰岩和页岩组成。等厚图和地层对比有助于了解野外隋主灰岩的厚度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reservoir Characterization of Eocene Carbonates of Central Indus Basin, Pakistan
The present study is based on petrophysical analysis of the Eocene Sui Main Limestone (SML) penetrated in wells of Qadirpur Gas Field, Central Indus Basin, Pakistan. The analyzed petrophysical property of SML includes shale volume, total porosity, effective porosity, water saturation, hydrocarbon saturation and net pay thickness. The result from the study shows that the Sui Main Limestone reservoir is capable of yielding appreciable hydrocarbon. The petrophysical interpretation revealed that the studied SML has productive reservoir characteristics with average (total and effective) porosity is in K-1, 15% in K-2 15% and 17% in K-3, average saturated hydrocarbon in SML is (70-100%) indicating that zones in wells are purely saturated with hydrocarbon, and average volume of shale in the zone of K-1, 23% in K2, 27% and in K-3, 25% respectively delineating clean formation. Facies modeling revealed that the studied Eocene formation consist of clean limestone, shaly limestone and shals. The isopach thickness map and stratigraphic correlation helps to understand the thickness of Sui Main Limestone in the field.
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