Abstract

The present study is focused on formation evaluation of the Lockhart Limestone in two wells (Meyal-05P and Meyal-10P) located in Northern Deformed Potwar Zone of the Potwar sub-basin, Pakistan. The geological formations ranging from Triassic to Pliocene have been drilled in these wells. The formation evaluation of the Lockhart Limestone mainly involves reservoir potential evaluation, interpretation of depositional environment and transgressive–regressive sequences using petrophysical logs. In either wells, the reservoir characterization is steered by various petrophysical parameters including calculation of volume of shale, porosity, permeability and hydrocarbon saturation. The thickness of the Lockhart Limestone is 50 m and 77 m in the Meyal-05P and Meyal-10P wells, respectively. In Meyal-05P and Meyal-10P wells, the average petrophysical parameters values and ranges are given as follows: volume of shale 48% and 20%; density porosity 1–5.6% and 1–31.7%; neutron porosity 1–23% and 1–42.9%; sonic porosity 1–29% and 1–39%; effective porosity < 1–> 5% and 1–21%; and hydrocarbon saturation 92.21–99.8% and 97–99.6%. The petrophysical parameters indicate that the Lockhart Limestone of Meyal-10P well is quantitatively better reservoir than that of the Meyal-05P. In Lockhart Limestone of either wells, the permeability is < 0.1 mD. The bulk volume water deciphered the presence of vuggy and intercrystalline porosity in the Lockhart Limestone. Similarly, the lithological interpretation using logs shows mainly limestone with minor shales. Different electrofacies are interpreted from the log trends of gamma ray log such as aggrading, prograding and retrograding depositional sequences deposited in tidal channel fill, shallow water, shore line and offshore buildup and regressive-to-transgressive shore face depositional setting.

Highlights

  • Meyal Oil Field is positioned in District Attock in an active foreland fold and thrust belt in the Potwar sub-basin of the Upper Indus Basin (Fig. 1; Hasany and Saleem 2012)

  • The Lockhart Limestone penetrated in Meyal-05P and Meyal-10P wells is investigated in the context of well logsbased reservoir evaluation, establishment of T–R sequences and interpretation of depositional environments

  • Different petrophysical logs have been run through this interval, and the following formation evaluation parameters are measured from these logs (Fig. 7)

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Summary

Introduction

Meyal Oil Field is positioned in District Attock in an active foreland fold and thrust belt in the Potwar sub-basin of the Upper Indus Basin (Fig. 1; Hasany and Saleem 2012). The Potwar sub-basin is an important hydrocarbon province of Pakistan and one of the mature areas explored for petroleum in the country (Kadri 1995). In 1915 at Khaur (District Attock), Punjab, commercial quantities of oil were discovered by the predecessor of Attock Oil Company (AOC) which founded the petroleum exploration history of the Potwar sub-basin (Kadri 1995). The Meyal Oil Field is one of the key oil producing fields in the Potwar sub-basin which includes 16 wells. It has produced over 36 MMB oil and 250 BCF gas from fractured Paleocene–Eocene shallow marine shelf carbonates of the Lockhart and Chorgali–Sakesar formations and Jurassic Datta sandstone (Hasany and Saleem 2012)

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